塔里木盆地东北缘早古生代造山带的构造特征、造山过程及对塔里木盆地的影响
|
摘要
塔里木盆地东北缘位于中亚造山带的南缘,经历复杂增生造山过程,是研究增生型造山带的理想场所。同时它又处于联结东天山造山带与塔里木盆地的特殊构造位置,是研究盆山耦合关系的一个重要区域。
作者结合野外考察与室内研究,对塔里木盆地东北缘造山带进行构造分析,结合年代学、岩石学、地球化学、地层学及沉积学等。对塔里木盆地东北缘造山带的造山过程以及与塔里木盆地的关系进行研究和探讨。主要研究成果及认识如下：
1)建立塔里木盆地东北缘造山带的基本构造格架。
根据南天山内榆树沟-铜花山缝合带及相邻单元之间大型韧性走滑剪切带(断裂)的空间位置,将塔里木盆地东北缘造山带划分为：(Ⅰ)北天山晚古生代增生体(NTSA)、(Ⅱ)中天山复合增生弧地块(CTSB)、(Ⅲ)南天山早古生代增生楔(STSA),及(Ⅳ)塔里木北部陆缘(NTRMM)(在研究区内主要指库鲁克塔格隆起)。它们之间的界限为中天山北缘剪切带(断裂)、中天山南缘剪切带(断裂)榆树沟-铜花山缝合带及辛格尔剪切带(断裂)。
2)确定塔里木盆地东北缘库鲁克塔格地区前南华纪的多次变质岩浆事件,发现前南华纪基底中存在一条大型韧性滑脱剪切带。塔里木盆地东北缘库鲁克塔格地区广泛出露前南华基底岩石。锆石LA-ICP-MS测试获得2505 Ma和1161～811 Ma的年龄,结合前人同位素测年结果,认为库鲁克塔格地区存在晚太古代-早元古代基底(2400-2800 Ma,或更老),经历元古代的1880-1817 Ma,1161～811 Ma的变质岩浆事件。库鲁克塔格地区基底与盖层之间存在一条E-W走向、厚度约2 km的韧性滑脱带,韧性滑脱带内普遍发育糜棱岩及“A”型剪切褶皱等,糜棱岩面理向N或S缓倾、拉伸线理向NW或SE倾伏,不对称旋转构造及糜棱岩中石英晶格优选方位图(EBSD测试)指示韧性滑脱带上盘滑脱方向为自NW向SE。韧性滑脱带中糜棱岩内白云母的Ar-Ar测年结果表明滑脱时代早于383 Ma。
3)确定库鲁克塔格震旦纪-早古生代岩石经历多期构造变形叠加。
库鲁克塔格震旦纪-早古生代岩石经历多期构造变形可分为4期：(1)N-S向挤压变形；(2)右行走滑韧脆性变形；(3)库鲁克塔格地区东部NE-SW向挤压变形与左行走滑韧脆性变形；(4)新生代陆内逆冲推覆和舒缓褶皱变形。
4)库鲁克塔格早古生代盖层由底部到顶部早期变形程度逐渐变弱。由N到S呈逆冲席状展布,向S逆冲推覆。采用层长守恒原理对震旦纪-早古生代盖层缩短率进行估算结果为19.0-22.1%。
5)塔里木盆地东北缘造山带中4条大型右行走滑剪切带(断裂)的厘定及形成时限的确认。
确定中天山北缘剪切带、中天山南缘剪切带、辛格尔剪切带以及兴地剪切带为韧性-脆性右行剪切带。塔里木盆地东北缘造山带中物质存在自西向东运动的轨迹。这些右行走滑剪切带形成于368～340 Ma (Ar-Ar测年结果),再次活动于290～241 Ma (Ar-Ar测年结果)。
6)确定塔里木盆地东北缘造山带中存在加里东造山事件。
塔里木盆地东北缘造山带中存在加里东造山事件,证据为：(1)中天山南缘存在一条早古生代的蛇绿岩带：榆树沟-铜花山蛇绿岩带；(2)库鲁克塔格寒武-奥陶系为早古生代被动陆缘深海-斜坡相沉积；(3)库米什地区出露古南天山洋盆的俯冲产物-早古生代深海沉积增生楔；(4)中天山广泛出露早古生代岩浆弧型花岗岩：(5)库鲁克塔格在早古生代形成向南逆冲极性的褶皱冲断带；(6)塔里木盆地东北缘造山带与盆地内发育有一定规模的志留-泥盆系砾岩；(7)以角度不整合接触的石炭系与奥陶系-志留系具有不同的构造变形特征,石炭系变形多为宽缓直立褶皱,而奥陶-志留系为具有流劈理的直立紧密褶皱；(8)库鲁克塔格“铲”式盖层与基底基底组成的滑脱-褶皱构造,是塔里木地块与中天山岩浆弧带碰撞(早于383 Ma)后发生陆内俯冲的产物。(9)由于碰撞后大型陆内平移作用引起的大型右行走滑剪切带在泥盆纪368-340 Ma(Ar-Ar测年结果)之前已经形成,说明开始在碰撞作用很可能发生在早古生代。
7)探讨了在加里东期塔里木盆地与塔里木盆地东北缘造山带之间存在相互制约的关系。
早古生代造山结束后,形成前陆盆地。以塔里木盆地东北缘造山带中以及塔里木盆地中普遍存在的早-中古生代砂岩、砂砾岩及泥质岩等为证据；碰撞造山后,盆-山结合部位发生陆内平移兼挤压。盆地内发生明显沉降。
8)提出塔里木盆地东北缘造山带的构造演化模式。
(1)震旦纪南天山洋开启；(2)震旦纪-早古生代,南天山洋盆收缩,塔里木地块开始向准噶尔地块俯冲,在中天山位置形成增生弧；(3)加里东期,塔里木地块与中天山增生岩浆弧带碰撞。形成一系列北倾南冲的不对称相似褶皱、北倾流劈理。同时形成磨拉石盆地,但这些盆地大部分仍在海平面以下；(4)弧-陆碰撞刚结束时,在塔里木盆地东北缘造山带处发生陆内平移兼逆冲过程,盖层与基底之间形成大规模韧性滑脱带；(5)受到北部古亚洲洋向S俯冲作用的影响,在塔里木盆地东北缘普遍发育石炭纪的具有弧后位置拉张裂解形成环境的火山岩；(6)早二叠世大规模沿造山带平行分布的陆相红色磨拉石(舒良树等,2004)是由于弧-陆碰撞造山而形成的磨拉石盆地由海相转为陆相的标志；(7)碰撞造山后二叠纪-早三叠世塔里木盆地东北缘造山带内发生大型右行韧脆性走滑；(8)受到阿尔金断裂系统的影响塔里木盆地东北缘造山带东部具有左行走滑的变形特征；(9)中生代在塔里木盆地东北缘造山带普遍发生大规模抬升剥蚀；(10)新生代由于印度板块向青藏高原挤压作用,塔里木盆地东北缘发生陆内再挤压再造山过程。
The northeastern margin of Tarim basin is located along the southern margin of the Central Asia Orogenic belt, has undergone an accretional orogenic process, connects the East Tianshan Orogen and Tarim Basin, it is an important area that geologists study accretion-type orogens and basin-mountain coupling relations.
With field investigation and lab study, the author analyzed the orogenic process of orogenic belt and its relations with Tarim Basin combining studies on structural geology, chronology, petrology, geochemistry, stratigraphy and sedimentology.
1) Establish structural framework of the orogenic belt on the northeastern margin of Tarim basin
According to the locations of Yushugou-Tonghuashan suture zone in South Tishan and large strike-slip ductile shear zones between neighboring units, orogenic belt in the northeastern margin of Tarim is divided into several parts including the North Tianshan unit, the Central Tianshan unit, the South Tianshan unit and the Kuruktag unit with the boundaries:the north Central Tianshan shear zone, the south Central Tianshan shear zone, Yushugou-Tonghuashan suture zone, Xinger shear zone and Xingdi shear zone.
2) Identify pre-Sinian metamorphic and magmatic events in Kuruktag, discover a large ductile detachment shear zone in the basement of the orogenic belt at the northeast Margin of Tarim Basin.
The basement rocks outcrop widely in Kuruktag. With zircon dating result of 2505 Ma and 1161-811 Ma and other previous isotope dating results, it is believed that Kuruktag terrane has late archean-early proterozoic (2565-2296 Ma) or older basement and experienced major metamorphic and magmatic events of proterozoic period at 1880-1817 Ma and 1161-811 Ma. (2) A decollement exists between the cover rocks and the basement stretches in E-W direction with a width of 2 km, is characterized by "A" type fold, mylonites, gently mylonite foliation, stretching lineation plunging to northwest or southeast. Studies on asymmetrical rotational structure and crystallographic preferred orientations of quartz in mylonites (EBSD analysis) indicate a movement of the ductile decollement in a top-to SE direction. (3) Ar-Ar dating result of the muscovite in the mylonite from the ductile decollement shows the decollement formed before 383 Ma.
3) Sinian-early Paleozoic rocks in orogenic belt in the northeastern margin of Tarim experienced several deformation envents.
The deformation events can be divided into 4 periods, including (1) N-S compressional deformation, (2) dextral strike-slip ductile-brittle deformation, (3) NE-SW compressional deformation and sinistral strike-slip ductile-brittle deformation in the east of this area, (4) intra-continental thrusting and gently folding deformation occurred in Cenozoic.
4) Early Paleozoic cap rocks thrusting southward spread sheet-like from N to S and are deformed weaker increasingly from bottom to top.
5) Redefine four large dextral strike-slip shear zones in orogenic belt of the northeastern margin of Tarim Basin and identify their formation duration time.
The north Central Tianshan shear zone, the south Central Tianshan shear zone, Xinger shear zone and Xingdi shear zone are identified as ductile-brittle dextral shear zones. These dextral strike-slip shear zones formed before 368-340 Ma (Ar-Ar dating results), and large scale Intra-continental ductile dextral strike-slipping event occurred at 290-241 Ma (Ar-Ar dating results).
6) Identify Caledonian orogenic event on the orogenic belt in the northeastern margin of Tarim, the northeastern margin of Tarim Basin.
The evidences are:(1) An early Paleozoic suture zone (Yushugou Tonghuashan suture zone) exists in the south Tianshan; (2) The Cambrian and Ordovician rocks in Kuruktag (south part of the orogeny) have the feature of passive continental margin abyssal and slope facies. (3) Early Paleozoic abyssal sedimentary accretionary wedge, the product of paleo South Tianshan Ocean subduction, outcrops in Kumish (in the south Tianshan). (4) Early Paleozoic magmatic arc-type granites outcrop widely in Central Tianshan. (5) Fold-thrust belt thrusting southward formed at early Paleozoic in Kuruktag. (6) Silurian-Devonian conglomerates develop widely in orogenic belt and basin, northeastern margin of Tarim Basin. (7) Carboniferous rocks and Ordovician-Silurian rocks contacted with an angular unconformity have different structural features. Deformation in Carboniferous rocks occur broad and gentle upright folds and Ordovician-Silurian upright compact folds with flow cleavage. (8) The spade-like cap rocks and the decollement bellow them is the product of the intercontinental subduction after the collision event (before 383 Ma). (9) Dextral strike-slip fault system in Central Tianshan and Kuruktag, the product of intra-continental deformation after early Paleozoic close of the south Tishan Ocean, formed at 368-340 Ma (Ar-Ar dating results).
7) The relation between Tarim Basin and the northeastern margin orogenic belt at the early paleogenic.
After early Paleozoic orogeny foreland basin formed and massive sandstone, sandy conglomerate and mudstone deposited. After collisional orogeny intra-continental translation and compression happened in basin-mountain binding site. Apparent subsidence occurred in basin.
8) Propose a structural evolution pattern of the orogenic belt on the northeastern margin of Tarim
(1) At Sinian the South Tianshan Ocean opened. (2) Paleo South Tianshan ocean shrinked at Sinian-early Paleozoic period and the Tarim block subducted underneath the Jungar block resulting accretionary arc formed at Central Tianshan. (3) At Caledonian Tarim block and Central Tianshan accretionary magma arc collided which lead to formation of a series of asymmetric similar folds and flow cleavages. Molasses basins formed at the same time, the majority part of which was still under the sea level. (4) After the end of arc-continental collision, intra-continental translational thrusting occurred at orogenic belt, and large ductile detachment belt formed between cap and basement. (5) Carboniferous igneous rocks, indicating formation setting of extensional cracking at back-arc, develop widely in northeastern margin of Tarim due to subduction southward of paleo Asia Ocean at north. (6) Early Permian massive continental red molasses along orogenic belt are the signal that molasse basins began to change from marine to continental. (7) At Permian-early Triassic, large dextral ductile-brittle strike slip happened in northeastern margin of Tarim. (8) The east part of orogenic belt in northeastern margin of Tarim shows deformation characteristics of sinistral strike slip. (9) During Mesozoic period large uplift erosion occurred commonly in the orogenic belt of northeastern margin of Tarim. (10) At Cenozoic, the northeastern margin of Tarim experienced intra-continental compressinal orogenic process again due to the compression of India plate towards Tibetan plateau.
作者结合野外考察与室内研究,对塔里木盆地东北缘造山带进行构造分析,结合年代学、岩石学、地球化学、地层学及沉积学等。对塔里木盆地东北缘造山带的造山过程以及与塔里木盆地的关系进行研究和探讨。主要研究成果及认识如下：
1)建立塔里木盆地东北缘造山带的基本构造格架。
根据南天山内榆树沟-铜花山缝合带及相邻单元之间大型韧性走滑剪切带(断裂)的空间位置,将塔里木盆地东北缘造山带划分为：(Ⅰ)北天山晚古生代增生体(NTSA)、(Ⅱ)中天山复合增生弧地块(CTSB)、(Ⅲ)南天山早古生代增生楔(STSA),及(Ⅳ)塔里木北部陆缘(NTRMM)(在研究区内主要指库鲁克塔格隆起)。它们之间的界限为中天山北缘剪切带(断裂)、中天山南缘剪切带(断裂)榆树沟-铜花山缝合带及辛格尔剪切带(断裂)。
2)确定塔里木盆地东北缘库鲁克塔格地区前南华纪的多次变质岩浆事件,发现前南华纪基底中存在一条大型韧性滑脱剪切带。塔里木盆地东北缘库鲁克塔格地区广泛出露前南华基底岩石。锆石LA-ICP-MS测试获得2505 Ma和1161～811 Ma的年龄,结合前人同位素测年结果,认为库鲁克塔格地区存在晚太古代-早元古代基底(2400-2800 Ma,或更老),经历元古代的1880-1817 Ma,1161～811 Ma的变质岩浆事件。库鲁克塔格地区基底与盖层之间存在一条E-W走向、厚度约2 km的韧性滑脱带,韧性滑脱带内普遍发育糜棱岩及“A”型剪切褶皱等,糜棱岩面理向N或S缓倾、拉伸线理向NW或SE倾伏,不对称旋转构造及糜棱岩中石英晶格优选方位图(EBSD测试)指示韧性滑脱带上盘滑脱方向为自NW向SE。韧性滑脱带中糜棱岩内白云母的Ar-Ar测年结果表明滑脱时代早于383 Ma。
3)确定库鲁克塔格震旦纪-早古生代岩石经历多期构造变形叠加。
库鲁克塔格震旦纪-早古生代岩石经历多期构造变形可分为4期：(1)N-S向挤压变形；(2)右行走滑韧脆性变形；(3)库鲁克塔格地区东部NE-SW向挤压变形与左行走滑韧脆性变形；(4)新生代陆内逆冲推覆和舒缓褶皱变形。
4)库鲁克塔格早古生代盖层由底部到顶部早期变形程度逐渐变弱。由N到S呈逆冲席状展布,向S逆冲推覆。采用层长守恒原理对震旦纪-早古生代盖层缩短率进行估算结果为19.0-22.1%。
5)塔里木盆地东北缘造山带中4条大型右行走滑剪切带(断裂)的厘定及形成时限的确认。
确定中天山北缘剪切带、中天山南缘剪切带、辛格尔剪切带以及兴地剪切带为韧性-脆性右行剪切带。塔里木盆地东北缘造山带中物质存在自西向东运动的轨迹。这些右行走滑剪切带形成于368～340 Ma (Ar-Ar测年结果),再次活动于290～241 Ma (Ar-Ar测年结果)。
6)确定塔里木盆地东北缘造山带中存在加里东造山事件。
塔里木盆地东北缘造山带中存在加里东造山事件,证据为：(1)中天山南缘存在一条早古生代的蛇绿岩带：榆树沟-铜花山蛇绿岩带；(2)库鲁克塔格寒武-奥陶系为早古生代被动陆缘深海-斜坡相沉积；(3)库米什地区出露古南天山洋盆的俯冲产物-早古生代深海沉积增生楔；(4)中天山广泛出露早古生代岩浆弧型花岗岩：(5)库鲁克塔格在早古生代形成向南逆冲极性的褶皱冲断带；(6)塔里木盆地东北缘造山带与盆地内发育有一定规模的志留-泥盆系砾岩；(7)以角度不整合接触的石炭系与奥陶系-志留系具有不同的构造变形特征,石炭系变形多为宽缓直立褶皱,而奥陶-志留系为具有流劈理的直立紧密褶皱；(8)库鲁克塔格“铲”式盖层与基底基底组成的滑脱-褶皱构造,是塔里木地块与中天山岩浆弧带碰撞(早于383 Ma)后发生陆内俯冲的产物。(9)由于碰撞后大型陆内平移作用引起的大型右行走滑剪切带在泥盆纪368-340 Ma(Ar-Ar测年结果)之前已经形成,说明开始在碰撞作用很可能发生在早古生代。
7)探讨了在加里东期塔里木盆地与塔里木盆地东北缘造山带之间存在相互制约的关系。
早古生代造山结束后,形成前陆盆地。以塔里木盆地东北缘造山带中以及塔里木盆地中普遍存在的早-中古生代砂岩、砂砾岩及泥质岩等为证据；碰撞造山后,盆-山结合部位发生陆内平移兼挤压。盆地内发生明显沉降。
8)提出塔里木盆地东北缘造山带的构造演化模式。
(1)震旦纪南天山洋开启；(2)震旦纪-早古生代,南天山洋盆收缩,塔里木地块开始向准噶尔地块俯冲,在中天山位置形成增生弧；(3)加里东期,塔里木地块与中天山增生岩浆弧带碰撞。形成一系列北倾南冲的不对称相似褶皱、北倾流劈理。同时形成磨拉石盆地,但这些盆地大部分仍在海平面以下；(4)弧-陆碰撞刚结束时,在塔里木盆地东北缘造山带处发生陆内平移兼逆冲过程,盖层与基底之间形成大规模韧性滑脱带；(5)受到北部古亚洲洋向S俯冲作用的影响,在塔里木盆地东北缘普遍发育石炭纪的具有弧后位置拉张裂解形成环境的火山岩；(6)早二叠世大规模沿造山带平行分布的陆相红色磨拉石(舒良树等,2004)是由于弧-陆碰撞造山而形成的磨拉石盆地由海相转为陆相的标志；(7)碰撞造山后二叠纪-早三叠世塔里木盆地东北缘造山带内发生大型右行韧脆性走滑；(8)受到阿尔金断裂系统的影响塔里木盆地东北缘造山带东部具有左行走滑的变形特征；(9)中生代在塔里木盆地东北缘造山带普遍发生大规模抬升剥蚀；(10)新生代由于印度板块向青藏高原挤压作用,塔里木盆地东北缘发生陆内再挤压再造山过程。
The northeastern margin of Tarim basin is located along the southern margin of the Central Asia Orogenic belt, has undergone an accretional orogenic process, connects the East Tianshan Orogen and Tarim Basin, it is an important area that geologists study accretion-type orogens and basin-mountain coupling relations.
With field investigation and lab study, the author analyzed the orogenic process of orogenic belt and its relations with Tarim Basin combining studies on structural geology, chronology, petrology, geochemistry, stratigraphy and sedimentology.
1) Establish structural framework of the orogenic belt on the northeastern margin of Tarim basin
According to the locations of Yushugou-Tonghuashan suture zone in South Tishan and large strike-slip ductile shear zones between neighboring units, orogenic belt in the northeastern margin of Tarim is divided into several parts including the North Tianshan unit, the Central Tianshan unit, the South Tianshan unit and the Kuruktag unit with the boundaries:the north Central Tianshan shear zone, the south Central Tianshan shear zone, Yushugou-Tonghuashan suture zone, Xinger shear zone and Xingdi shear zone.
2) Identify pre-Sinian metamorphic and magmatic events in Kuruktag, discover a large ductile detachment shear zone in the basement of the orogenic belt at the northeast Margin of Tarim Basin.
The basement rocks outcrop widely in Kuruktag. With zircon dating result of 2505 Ma and 1161-811 Ma and other previous isotope dating results, it is believed that Kuruktag terrane has late archean-early proterozoic (2565-2296 Ma) or older basement and experienced major metamorphic and magmatic events of proterozoic period at 1880-1817 Ma and 1161-811 Ma. (2) A decollement exists between the cover rocks and the basement stretches in E-W direction with a width of 2 km, is characterized by "A" type fold, mylonites, gently mylonite foliation, stretching lineation plunging to northwest or southeast. Studies on asymmetrical rotational structure and crystallographic preferred orientations of quartz in mylonites (EBSD analysis) indicate a movement of the ductile decollement in a top-to SE direction. (3) Ar-Ar dating result of the muscovite in the mylonite from the ductile decollement shows the decollement formed before 383 Ma.
3) Sinian-early Paleozoic rocks in orogenic belt in the northeastern margin of Tarim experienced several deformation envents.
The deformation events can be divided into 4 periods, including (1) N-S compressional deformation, (2) dextral strike-slip ductile-brittle deformation, (3) NE-SW compressional deformation and sinistral strike-slip ductile-brittle deformation in the east of this area, (4) intra-continental thrusting and gently folding deformation occurred in Cenozoic.
4) Early Paleozoic cap rocks thrusting southward spread sheet-like from N to S and are deformed weaker increasingly from bottom to top.
5) Redefine four large dextral strike-slip shear zones in orogenic belt of the northeastern margin of Tarim Basin and identify their formation duration time.
The north Central Tianshan shear zone, the south Central Tianshan shear zone, Xinger shear zone and Xingdi shear zone are identified as ductile-brittle dextral shear zones. These dextral strike-slip shear zones formed before 368-340 Ma (Ar-Ar dating results), and large scale Intra-continental ductile dextral strike-slipping event occurred at 290-241 Ma (Ar-Ar dating results).
6) Identify Caledonian orogenic event on the orogenic belt in the northeastern margin of Tarim, the northeastern margin of Tarim Basin.
The evidences are:(1) An early Paleozoic suture zone (Yushugou Tonghuashan suture zone) exists in the south Tianshan; (2) The Cambrian and Ordovician rocks in Kuruktag (south part of the orogeny) have the feature of passive continental margin abyssal and slope facies. (3) Early Paleozoic abyssal sedimentary accretionary wedge, the product of paleo South Tianshan Ocean subduction, outcrops in Kumish (in the south Tianshan). (4) Early Paleozoic magmatic arc-type granites outcrop widely in Central Tianshan. (5) Fold-thrust belt thrusting southward formed at early Paleozoic in Kuruktag. (6) Silurian-Devonian conglomerates develop widely in orogenic belt and basin, northeastern margin of Tarim Basin. (7) Carboniferous rocks and Ordovician-Silurian rocks contacted with an angular unconformity have different structural features. Deformation in Carboniferous rocks occur broad and gentle upright folds and Ordovician-Silurian upright compact folds with flow cleavage. (8) The spade-like cap rocks and the decollement bellow them is the product of the intercontinental subduction after the collision event (before 383 Ma). (9) Dextral strike-slip fault system in Central Tianshan and Kuruktag, the product of intra-continental deformation after early Paleozoic close of the south Tishan Ocean, formed at 368-340 Ma (Ar-Ar dating results).
7) The relation between Tarim Basin and the northeastern margin orogenic belt at the early paleogenic.
After early Paleozoic orogeny foreland basin formed and massive sandstone, sandy conglomerate and mudstone deposited. After collisional orogeny intra-continental translation and compression happened in basin-mountain binding site. Apparent subsidence occurred in basin.
8) Propose a structural evolution pattern of the orogenic belt on the northeastern margin of Tarim
(1) At Sinian the South Tianshan Ocean opened. (2) Paleo South Tianshan ocean shrinked at Sinian-early Paleozoic period and the Tarim block subducted underneath the Jungar block resulting accretionary arc formed at Central Tianshan. (3) At Caledonian Tarim block and Central Tianshan accretionary magma arc collided which lead to formation of a series of asymmetric similar folds and flow cleavages. Molasses basins formed at the same time, the majority part of which was still under the sea level. (4) After the end of arc-continental collision, intra-continental translational thrusting occurred at orogenic belt, and large ductile detachment belt formed between cap and basement. (5) Carboniferous igneous rocks, indicating formation setting of extensional cracking at back-arc, develop widely in northeastern margin of Tarim due to subduction southward of paleo Asia Ocean at north. (6) Early Permian massive continental red molasses along orogenic belt are the signal that molasse basins began to change from marine to continental. (7) At Permian-early Triassic, large dextral ductile-brittle strike slip happened in northeastern margin of Tarim. (8) The east part of orogenic belt in northeastern margin of Tarim shows deformation characteristics of sinistral strike slip. (9) During Mesozoic period large uplift erosion occurred commonly in the orogenic belt of northeastern margin of Tarim. (10) At Cenozoic, the northeastern margin of Tarim experienced intra-continental compressinal orogenic process again due to the compression of India plate towards Tibetan plateau.
引文
Allen M B, Windley B F, Zhang C.1992. Palaeozoic collisional tectonics and magmatism of the Chinese Tien Shan, central Asia. Tectonophysics 220:89-115
Allen M B, Windley B F, Zhang C.1994. Cenozoic tectonics in the Urumqi-Korla region of the Chinese Tianshan. Geol Rundsch,83:406-416
Andrsen T.2002. Correction of common lead in U-Pb analyses that do not report 204Pb. Chemical Geology,192:59-79
Bacon G R and Druit T H.1988. Compositional evolution of the zoned talc-alkaline magna chamber of Mount Mazama, Crater Lake, Oregon. Contrib. Mineral. Petrol.,98:224-256
Bhatia M R.1983. Plate tectonics and geochemical composition of sandstones. Journal of Geology,91:611-627
Brookfield M E.2000. Geological development and Phanerozoic crustal accretion in the western segment of the southern Tianshan (Kyrgyzstan, Uzbekistan and Tagikistan). Tectonophysics,328:1-14
Bullen M E, Burbank D W, Garver J I.2001. Late Cenozoic tectonic evolution of the northwestern Tian Shan New age estimates for the initiation of mountain building DSR bulletin.113(12):1544-1559
Burchfiel B C, Royden L H.1991. Tectonics of Asia 50 years after the death of Emile Argand. Eclogae Geol Helv,84:599-629
Busby C J, Ingersoll R V.1995. Tectonics of sedimentary basins.Oxford:Blackwell Science
Chen C, Lu H, Jia D, et al.1999. Closing history of the southern Tianshan oceanic basin, western China:an oblique collisonal orogeny. Tectonophysics,302: 23-40.
Christiansen R L.1984. Yellowstone magmatie evolution; its bearing on understanding large volume explosive volcanism. In Explowive Volcanism; Inception, evolution and hazards. National Academy Press, Washington D C, 84-95
Cloetingh S, Ben Avraham Z, Sassi W, Horvath F.1996. Dynamics of Extensional Basins and inversion Tectonics. Tectonophysics,266:1-523
Cloetingh S, Eldholm O, Larsen B T, Gabrielsen R, Sassi W.1994. Dynamics of Extensional Basin Formation. Tectonophysics,240:1-341
Cloetingh S, Sassi W, Hoevath F.1993. The origin of Sedimentary Basins:Inferences from Quantative Modelling and Basin Analysis. Tectonophysics,226:1-518
Dewey J F, Bird J M.1970. Mountain belts and new global tectonic. Geophys Res,75: 2625-2647
Ernst W G. 2005. Alpine and Pacific styles of Phanerozoic mountain building: subduction zone petrogenesis of continental crust.Tarra Nova,17:165-188
Gao J, Klemd R.2003. Formation of HP-LT rocks and their tectonic implications in the western Tianshan Orogen, NW China:geochemical and age constraints. Lithos,66:1-22
Gao J, Li M S, Xiao X C, Tang Y Q, He G Q.1998. Paleozoic tectonic evolution of the Tianshan orogen, northwestern China. Tectonophysics,287:213-231
Gao J, Long L L, Klemd R, Qian Q et al.2009. Tectonic evolution of the south Tianshan orogen and adjacent regions, NW China:geochemical and age constraints of granitoid rocks. Int. J. Earth Scie. (Geol Rundsch),98:1221-1238
Gao J, He G Q, Li M S, Xiao X C, Tang Y Q, Wang J, Zhao M.1995. The mineralogy,petrology,metamorphic PTDt trajectory and exhumation mechanism of blueschists,south Tianshan, northwestern China. Tectonophysics 250:151 168
Gao J, Klemd R, Qian Q, Zhang X, et al.2011. The collision between the Yili and Tarim blocks of the Southwestern Altaids:Geochemical and age constraints of a leucogranite dike crosscutting the HP-LT metamorphic belt in the Chinese Tianshan Orogen. Tectonophysics. impress.
Grove T L and Donnelly-Nolan M.1986. The evolution of young sillic lavas at Medicine Lake volcano, California:implications for the origin of compositional gaps in calc-alkaline series lavas. Contrub. Mineral. Petol.,92 (2):281-302
Hsu K J, Yao Y, Hao J, Hsu P, Li J andWangO.1994. Origin ofChinese Tianshan by arc-arc collisions. Eclogae GolHelv,87(1):65-292
Hu A Q, Jahn B M, Zhang G X, Chen Y B, Zhang Q F.2000. Crustal Evolution and Phanerozoic Crustal Growth in Northern Xinjiang:Nd Isotopic Evidence. Part Ⅰ: Isotopic Characterization of Basement Rocks. Tectonophysics,15-51
Hu A Q, Rogers G. 1992. Discovery of 3.3 Ga Archean rocks in north Tarim Block of Xinjiang, western China. Chinese Science Bulletin,37 (18):1546-1549
Huton D H W, Reavy R J.1992. Strike-slip tectonics and granite petrogenesis.Tectonics,11:960-967
Jahn B m, Windley B, Natalin, B, et al.2004. Phanerozoic continental growth in Central Asia. Journal of Asian Earth Sciences,23:599-603
Koppers A A P.2002. Software for 39Ar/40Ar age calculations. Computers and Geosciencs,28:605-619
Kroner A., Windley B F, Badarch G, Tomurtogoo O, Hegner E, Jahn B M, Gruschka S, Khain E V, Demoux A, Wingate M T D.2007. Accretionary growth and crustformation in the central Asian Orogenic Belt and comparison with the Arabian-Nubian shield. In:Hatcher Jr., R.D., Carlson, M.P., McBride, J.H., Martinez Catalan, J.R. (Eds.),4-D Framework of Continental Crust: Geological Society of America Memoir,200, p.181-209.10.1130/2007.1200(11).
Laurent-Charvet S, Charvet J, Shu L S, Ma R S and Lu H E.2002. Paleozoic late collisional strikeslip dcformations in Tianshan and Altay, Eastern Xinjiang, NW China. Terra Nova,14:245-256
Laurent-Charvet S, Charvet J, ShuLS, et al.2002. Ductile strike-slip shear zones in Eastern Xinjiang, NW China:ALate Palaeozoic late collisional intracontinental adjustment. Terra Nova,14 (4):249-256
Laurent-Charvet S, MonieP, Charvet J, et al.2003. Late-Paleozoic strike-slip shear zones in northeastern Xinjiang (NW China):new structural and geochronological data. Tectonics,22 (2):1009-1032
Le Bas M J, Le Maitre R W, Streckeisen A, et al.1986. A chemical classification of volcanic rocks based on the total alkali-silica diagram. Journal of Petrology,27: 745-750
Li Y J, Sun L D, Wu H R, Zhang G Y, Wang G L, Huang Z B.2005. Permo Carboniferous radiolarians from the Wupata' erkan group, Western South Tianshan, Xinjiang, China. Acta Geologica Sinica,79 (1):16-23
Li Y J, Wang Z M, Wu H R, Huang Z B, Tan Z J, Luo J C. 2002. Discovery of radiolarian fossils from the Aiketik group at the western end of the South Tianshan Mountains of China and its implications. Acta Geologica Sinica, 76 (2): 146-154
Liu Y L, Zhang Z C, Guo Z J, Huang B L, Mu Z G. 1999. K Ar isochron dating of Kuluktag mafic dykes, Xinjiang autonomous region, and discussion on some related questions. Geological Journal of China Universities,5 (1):55-58
Liu Y S, Hu Z C, Gao S, Gunther D, Xu J, Gao C, Chen H.2008. In situ analysis of major and trace elements of anhydrous minerals by LA-ICP-MS without applying an internal standard. Chemical Geology,257:34-43
Liu Y, Hao S G. 2006. Evolutionary significance of pylentonemid radiolarians and their Late Devonian species from southwestern Tianshan, China. Acta Geologica Sinica,80 (5):647-655
Liu Y.2001. Early Carboniferous radiolarian fauna from Heiyingshan South of the Tianshan Mountains and its geotectonic significance. Acta Geologica Sinica,75 (1):101-108
Luddwig K R.1991. Isoplot-aplotting and regression program for radiogenic-isotope data. U S Geological Survey Open-file report,39:91-445
Ludwig K R.1991. ISOPLOT:A Plotting and Regression Program for Radiogenic isotope Data. US Geological Survey Open File Report, p.1-39
Mossakovsky A A, Ruzhentsev S V, Samygin S G, Kheraskova T N.1993. The Central Asian fold belt:geodynamic evolution and formation history. Geotectonics,26: 455-473
Price R A, Mountjoy E W.1971. Geologic structure of the Canadian Rocky Mountains between Bow and Athabasca Rivers a progress report. In:Wheeler JO (ed). Structure of the southern Canadian Cordillera:GeologicalAssociation ofCanada SpecialPaper,6:7-26
Reavy R J.1989. Structural controls on metamorphism and syntectonic magmatism: the Portuguese Hercynian collision belt. Journal of Geology Society London,146: 649-657
Ring U, Kroner A, Layer P, et al.1999. Deformed A-type granites in norther Malawi, east-central Africa:pre-or syntectonic? Jounal of the Geological Society, London,156:695-714
Roser B P, Korsch R J.1986. Determination of tectonic setting sandstone-mudstone suites using SiO2 content and K2O/Na2O ratio. Journal of Geology,94 (5): 635-650
Rurn J P, Cobbold P R.1980. Strain heating and thermal softening incontinental shear zones:a review.Journal of Structural Geology,2:149-158
Schumm S A, Dumont J F.2000. Active tectonics and alluvial rivers. Cambridge: Cambridge University Press, p.1-276
Sebastien Laurent-Charvet, Jacques Charvet, Liangshu Shu, Ruishi Ma, Huafu Lu. 2002. Palaeozoic late collisional strike-slip deformations in Tianshan and Altay, Eastern Xinjiang, NW China. Terra Nova,14 (4):249-256.
Sebastien Laurent-Charvet, Jacques Charvet, Patrick Monie, Liangshu Shu. Late Paleozoic strike-slip shear zones in eastern central Asia (NW China):New structural and geochronological data. Tectonics, doi:10.1029/2001TC901047.
Sengor A M C, Natal'in B A., Burtman V S.1993. Evolution of the Altaid tectonic collage andm Palaeozoic crustal growth in Eurasia. Nature,364:299-307
Sengor A M C, Natal'in B A.1996. Paleotectonics of Asia: fragments of a synthesis.In: Yin A, et al., eds. The Tectonic Evolution of Asia.Cambridge:Cambridge University Press, p.486-640
Sengor A M C.1990. Plate tectonics and orogenic research after 25 years:a Tethya perspective.Earth Science Reviewe,27:1-201
Sengor A M C.1992.板块构造学与造山运动-特提斯例析.丁晓翻译,上海.复旦大学出版社,p.1-182
Sengor A M C., Natalin B.1996. Turkic-type orogeny and its role in the making of the continental crust. Annual Reviews of Earth and Planetary Sciences,24: 263-337
Shu L S, Charvet J, Guo L Z, et al.1999. Laurent-Charvet Sebastien. A large-scale Palaeozoic dextral ductile strike-slip zone:the Aqqikkudug-Weiya zone along the northern margin of the Central Tianshan belt, Xinjiang, NW China. Acta Geol. Sinica,73 (2):148-162
Shu L S, Charvet J, Lu H F, et al.2002. Paleozoic accretion-collision events and kinematicsof ductile deformation in the central-southern Tianshan Belt, China. Acta Geol. Sinica,76 (3):308-323
Shu L S, Charvet J, Ma R S.1998. Study of a large scale Paleozoic dextral strike-slip ductile shear zone along the northern margin of the central Tianshan, Xinjiang. Xinjiang Geology,16 (4):326-336
Sun S S, Mcdonough W F.1989. Chemical and isotopic systematics of oceanic basalts: implications for mantle composition and Processes.Saunders A D, Norry M J. Magmatism in the Ocean Basins. London:Geol. Soc. Spec. Pub.,42:313-45
Tapponnier P, Peltzer G, Armijo R.1986. On the mechanics of the collision between India and Asia. Geol Soc Spec Publ,19:115-157
Wang X W, Chen F J.1997. Sinian-Ordovician tectonic evolution of north Tarim and south Tianshan region and its relation to oil and gas. Geoscience-Journal of Graduate School, China University of Geoscience,11 (3):313-321
Willson W.1989. Igneous petrogenesis. Unwin Hyman, London, p.327-373
Wilson J T.1990. On the building and classification of Mountains. J Geophys Res,95: 6611-6628
Windley B F, Alexeiev D, Xiao W, Kroner A, Badarch G 2007. Tectonic models for accretion of the Central Asian Orogenic belt. Journal of the Geological Society, London,164:31-47
Windley BF, Allen MB, Zhang C, Zhao Z, Wang Q.1990. Paleozoic accretion and Cenozoic redeformation of the Chinese Tien Shan range,central Asia.Geology,18: 128-131
Xiao W J, Han C M, Yuan C, Sun M, Lin S F, Chen H L, Li Z L, Li J L, Sun S.2008. Middle Cambrian to Permian subduction-related accretionary orogenesis of Northern Xinjiang, NW China:Implications for the tectonic evolution of central Asia. Journal of Asian Earth Sciences,32:102-117
Xiao W J, Huang B C, Han C M, Sun S, Li J L.2010. A review of the western part of the Altaids:A key to understanding the architecture of accretionary orogens. Gondwana Research,18 (2-3):253-273
Xiao W J, Zhang L C, Qin K Z, Sun S, Li J L.2004. Paleozoic accretionary and collisional tectonics of the eastern Tianshan (China):Implications for the continental growth of Central Asia. American Journal of Science,304:370-395
Xu B, Xiao S H, Zou H B, Chen Y, et al.2009. SHRIMP zircon U-Pb age constraints on Neoproterozoic Quruqtagh diamictites in NW China,168:247-258
Xu B, Zhang H, Yao H, Li Y.2003. Gisotopeeom sitionand signifieanee of the Sinianon theTarim Plate. Chinese Science Bullitin,48:385-389
Yang T N, Wang Y, Li J Y, Sun G H.2007. Vertical and horizontal strain partitioning of the Central Tianshan (NW China):Evidence from structures and 40Ar/39Ar geochronology. Journal of Structural Geology,29:1605-1621
Yin A, Nie S. Craig P and Harrison T M.1998. Late Cenozoic tectonic evolution of the South Chinese Tian Shan. Tectonics,17(1):1-27
Zhang L, Ai Y L, Li X P, Rubatto D, Song B, Williams S, Song S G, Ellis D, Liou J G.2007. Triassic collision of western Tianshan orogenic belt, China: Evidence from SHRIMP U-Pb dating of zircon from HP/UHP eclogitic rocks. Lithos,96:266-280
蔡东升,卢华复.1996.南天山蛇绿混杂岩和中天山南缘糜棱岩的40Ar/39Ar年龄及其大地构.地质科学,31(4)：384-390
车自成,刘洪福,刘良等.1994.中天山造山带的形成与演化.北京：地质出版社,p.1-142
陈汉林,杨树锋,董传万,贾承造,魏国齐,汪振国.1997.塔里木盆地二叠纪基性岩带的确定及大地构造意义.地球化学,26(6)：77-86
陈文,孙枢,张彦等.2005.新疆东天山秋格明塔什-黄山韧性剪切带40Ar/39Ar年代学研究.地质学报,79(6)：790-804
成守德,王元龙.1998.新疆大地构造演化基本特征.新疆地质,16(2)：97-107
程日辉,王璞,孙晓猛,白云风.2006.库鲁克塔格地区奥陶系层序地层与海平面变化.大地构造与成矿学,30(3)：283-293
邓松涛,郭召杰,张志诚,廖国辉.2006.南天山中段桑树园子韧性剪切带的形成时限及其构造意义.中国地质,33(3)：641-647
邓兴梁,舒良树,朱文斌,马东升,王博.2008.新疆兴地断裂带前寒武纪构造—岩浆—变形作用特征及其年龄.岩石学报,24(12)：2800-2808
地质部新疆维吾尔自治区地质局.1965.1：20万辛格尔幅地质图说明书.乌鲁木齐：新疆印刷厂
丁振举,姚书振,周宗桂等.2003.碧口群不同岩片火山岩微量元素组成差异与古构造意义,地球科学-中国地质大学学报,20(2)：167-172
董云鹏,王润三,周鼎武.2001.南天山北缘榆树沟变质基性超基性岩的地球化学及其成因机制.地球化学,30(6)：559-568
董云鹏,张国伟,周鼎武,罗金海,张成立,夏林圻,徐学义,李向民.2005.中天山北缘冰达坂蛇绿混杂岩的厘定及其构造意义.中国科学D辑：地球科学,35(6)：552-560
范璞,马宝林.1990.塔里木油气地质总论.北京：科学出版社,p.1-258
冯益民,朱宝清,杨军录等.2002.东天山大地构造及演化-1：50万东天山大地构造图简要说明.新疆地质,20(4)：309-314
高俊,龙灵利,钱青,黄德志,苏文.2006.南天山：晚古生代还是三叠纪碰撞造山带.岩石学报,22(5)：1049-1061
高俊,钱青,龙灵利,张喜,李继磊,苏文.2009.西天山的增生造山过程.28(12)：1804-1816
高俊,肖序常,汤耀庆,赵民,王军,吴汉泉.1993.南天山库米什蓝片岩的发现及其大地构造意义.中国区域地质,4：344-347
高锐,肖序常,高弘.2002.西昆仑-塔里木-天山岩石圈深地震探测综述.地质通报,21(1)：11-18
高振家,陈晋镳,陆松年,彭昌文等.1993.新疆北部前寒武系.前寒武纪地质第六号.北京：地质出版社
高振家,王务严,彭昌文等.1985.新疆震旦系(新疆地层总结之一).乌鲁木齐：新疆人民出版社,p.35-73
郭令智,施央申,卢华复.1992.印藏碰撞的两种远距离构造效应.现代地质学研究文集(上).南京：南京大学出版社,p.81-91
郭召杰,韩宝福,张志诚,邓松涛,刘畅.2007.中天山东段古生代淡色花岗岩的发现及其构造意义.岩石学报,23(8)：1841-1846
郭召杰,张志诚,廖国辉.2002.天山东段隆升过程的裂变径迹年龄证据及构造意义.新疆地质,20(4)：331-334
郭召杰,马瑞士,郭令智,施央申.1993.新疆东部三条蛇绿混杂带的比较研究.地质论评,39(3)：236-247
韩宝福,何国琦,吴泰然,李惠民.2004.天山早古生代花岗岩锆石U-Pb定年、岩石地球化学特征及其大地构造意义.新疆地质,22(1)：4-11
何登发,李德生.1996.塔里木盆地构造演化与油气聚集.北京：地质出版社,p.1-173
何国琦,李茂松,韩宝福.2001.中国西南天山及邻区大地构造研究.新疆地质,19(1)：7-11
何国琦,李茂松,刘德权,唐延龄,周汝洪.1994.中国新疆古生代地壳演化及成矿.乌鲁木齐：新疆人民出版社；香港：香港文化教育出版社,p.1-437
胡霭琴,王中刚,涂光炽等.1997.新疆北部地质演化及成矿规律.北京：科学出版社,p.9-35
胡霭琴,韦刚建.2006.塔里木盆地北缘新太古代辛格尔灰色片麻岩形成时代问题,地质学报,80(1)：126-133
胡霭琴,韦刚健,张积斌,邓文峰,陈林丽.2007.天山东段天湖东片麻状花岗岩的锆石SHRIMP U-Pb年龄和构造演化意义.岩石学,23(8)：1795-1802
胡霭琴,张国新,陈义兵等.2001.新疆大陆基底分区模式和主要地质事件的划分.新疆地质,19(1)：12-19
胡霭琴,张国新,张前锋,陈义兵.1999.天山造山带基底时代和地壳增生的Nd同位素制约.中国科学D辑：地球科学,29(2)：104-112
胡霭琴,张国新等.1995.新疆北部主要地质事件同位素年表,地球化学,24(1)：20-31
胡受奚,郭继吞,顾连兴等.1990.加里东造山带在东天山(E85°-90°),构造格架中的重要地位及其地质特征.新疆地质科学,地质出版社,32-46
黄汲清.1990.新疆及邻区板块开合构造及手风琴式运动.新疆地质科学,(1)：3-16
贾承造,姚慧君,魏国齐.1995.塔里木盆地板块构造演化和主要构造单元地质构造特征.北京：石油工业出版社,p.45-280
姜常义,姜寒冰,叶书锋,夏明哲,逯东霞.2005.新疆库鲁克塔格地区二叠纪岩脉群岩石地球化学特征,Nd、Sr、Pb同位素组成与岩石成因.地质学报,79(6)：823-833
姜常义,吴文奎,李良辰.2001.南天山东段显生宙构造演化.北京：地质出版社,1-160
姜常义,杨复,吴文奎,李良辰.1990.库米什地区火山岩岩石地球化学特征及大地构造环境,西安地质学院学报,12(1)：1-8
姜常义等,2001.天山地区新元古代-早寒武世火山岩地球化学和岩石成因.岩石矿物学杂志,25(5)：412-422
金文正,汤良杰,王清华,余一欣,万桂梅,杨文静,彭更新,雷刚林.2007.库车前陆盆地东秋里塔格构造带构造分段特征.大地构造与成矿学,31(3)：300-307
康玉柱.1993.塔里木盆地形成演化及构造特征与油气关系.新疆地质,11(2)：95-107
李春昱,王荃.1983.我国北部边陲及邻区的古板块构造与欧亚大陆的形成.见中国北方板块构造文集(1).北京：地质出版社
李海兵,杨经绥,许志琴,孙知明等.2006.阿尔金断裂带对青藏高原北部生长、隆升的制约.地学前缘,13(4)：59-79
李华芹,陈富文,蔡红,刘后群.1999.新疆东部马庄山金矿成矿作用同位素年代学研究.地质科学,34(2)：251-256
李继亮,孙枢,郝杰,陈海泓,侯泉林,肖文交,吴继敏.1999.碰撞造山带的碰撞事件时限的确定.岩石学报,15(2)：315-320
李继亮.1989.准噶尔残留弧后盆地与中天山造山带的大地构造关系.沉积学报,7(增刊)：53-61
李锦轶,何国琦,徐新等.2006.新疆北部及邻区地壳构造格架及其形成过程的初步探讨.地质学报,80(1)：148-168
李锦轶,王克卓,李亚萍,孙桂华,褚春华,李丽群,朱志新.2006.天山山脉地貌特征、地壳组成与地质演化.地质通报,25(8)：895-909
李锦轶.2004.新疆东部新元古代晚期至古生代的构造格局与构造演化.地质论评,50(3)：304-322
李伍平,王涛,李金宝,康旭,于福生,韩庆军,马忠平.2001.东天山红柳河地区海西期花岗岩的岩石学、地球化学及其构造环境.地质论评,47(4)：368-376
李向东,肖文交,周宗良.2004.南天山南缘晚泥盆世构造事件的40Ar/39Ar定年证据及其意义.岩石学报,20(3)：691-696
李向民,夏林圻,夏祖春,徐学义,马中平.2006.天山地区新元古代-早寒武世火山岩地球化学和岩石成因.岩石矿物学杂志,25(5)：412-422
李曰俊,孙龙德,吴浩若,张光亚,王国林,黄智斌.2004.南天山西段库尔干地区三叠纪砾岩的硅岩砾石中发现放射虫化石.地质科学,39(2)：153-158
李曰俊,王招明,周黎霞.2000.塔里木盆地西北部乌什地区构造单元划分和盆山耦合关系.见：王福同主编,第四届天山地质矿产资源学术讨论会论文集.乌鲁木齐：新疆人民出版社,p.27-30
李曰俊,杨海军,赵岩,罗俊成,郑多明,刘亚雷.2009.南天山区域大地构造与演化.大地构造与成矿学,33(1)：94-104
刘畅,赵泽辉,郭召杰.2006.甘肃北山地区煌斑岩的年代学和地球化学及其壳幔作用过程讨论.岩石学报,22(5)：1294-1306
刘训,吴绍祖,傅德荣,姚建新,丁孝忠,王永.1997.塔里木板块周缘的沉积-构造演化.新疆：新疆科技卫生出版社,p.1-256
刘玉琳,张志诚,郭召杰,黄宝玲,穆志国.1999.库鲁克塔格基性岩墙群K-Ar等时年龄测定及其有关问题讨论.高校地质学报,5(1)：55-58
卢德源,李秋生,高锐等.2000.横跨天山的人工爆炸地震剖面.科学通报,45(9)：982-988
卢华复,贾东,蔡东升,吴世敏.1996.塔里木与西天山板块构造演化.见：童晓克,梁狄刚,贾承造主编.塔里木盆地石油地质研究新进展.北京：科学出版社,p.235-245
卢华复,王胜利,贾东,王良书,刘绍文.2005.塔里木盆地与天山山脉晚新生代盆山耦合机制,高校地质学报,11(4)：493-503
卢华复,王胜利,罗俊成等.2006.塔里木盆地东部断裂系统及其构造演化.石油与天然气地质,27(4)：433-441
陆松年,李怀坤,陈志宏.2003.塔里木与扬子新元古代热构造事件特征、序列和时代—扬子与塔里木连接(ABCDEF)假设.地学前缘,10(4)：321-326
陆松年等编著.2006.中国前寒武纪重大地质问题研究：中国西部前寒武纪重大地质事件群及其全球构造意义.地质出版社.
罗新荣,石福品,樊卫东,罗新涛.2007.新疆库鲁克塔格新元古代花岗岩年龄和地球化学.资源调查与环境,28(4)：235-241
马华东,贺卫东,涂其军,陈静,曹福根,任燕.2008.新疆东天山地区塔水河韧性剪切带特征.大地构造与成矿学,32(1)：1-10
马瑞士,王赐银,叶尚夫等.1993.东天山构造格架及地壳演化.南京：南京大学出版社,p.1-225
马杏垣.2004.解析构造学.北京：地质出版社,p.1-463
潘家伟,李海兵,Jerome Van Der Woerd,孙知明.2007.西昆仑山前冲断带晚新生代构造地貌特征.地质通报,26(10)：1368-1379
任战利,肖晖,韩伟,梁宇,卿颖,腾志宏,史政.2009.孔雀河斜坡与库鲁克隆起构造-热演化史研究.39(3)：510-516
石玉若,刘敦一,张旗,简平,张福勤,苗来成.2006.中天山干沟一带花岗质岩类SHRIMP年代学及其构造意义.科学通报,51(22)：2665-2672
舒良树,郭召杰,朱文斌,卢华复,王博.2004.天山地区碰撞后构造与盆山演化.高校地质学报,10(3)：393-404
舒良树,卢华复,印栋豪,王博.2003.中、南天山古生代增生-碰撞事件和变形运动学研究.南京大学学报(自然科学版),39(1)：17-30
舒良树,王博,朱文斌.2007.南天山蛇绿混杂岩中放射虫化石的时代及其构造意义.地质学报,81(9)：1161-1168
舒良树,夏飞雅克,马瑞士.1998.中天山北缘大型右旋走滑韧剪带研究.新疆地质,16(4)：326-336
舒良树,朱文斌,王博,Faure M, Charvel J, Cluzel D.2005.新疆博格达南缘后碰撞期陆内裂谷和水下滑塌构造.岩石学报,21(1)：25-36
舒良树和卢华复.2003.中国中南天山造山带东段古生代增生-碰撞事件和韧性变形的运动学.南京大学学报(自然科学),39(1)：17-31
孙晓猛,王璞瑶,刘鹏举,郝福江.2006.兴地断裂构造特征及其演化历史.新疆地质,24(4)：348-352
汤良杰.1997.略论塔里木古生代盆地演化.现代地质,11(1)：14-20
汤耀庆,高俊,赵民,李锦轶,王军.1995.西南天山蛇绿岩和蓝片岩.北京：地质出版社,p.1-133
唐俊华,顾连兴,张遵忠,吴昌志等.2007.东天山咸水泉片麻状花岗岩特征、年龄及成因.23(8)：1803-1820
唐俊华,顾连兴,郑远川,方同辉,张遵忠,高军辉,王福田,汪传胜,张光辉.2006.东天山卡拉塔格钠质火山岩岩石学、地球化学及成因.岩石学报,2(5)：1150-1166
田纳新,程喆,陈文礼,林学庆.2008.塔里木盆地孔雀河地区构造变形特征及其控油气作用.石油实验地质.30(3)：236-241
田纳新,于明德,涂志民,马玉春.2005.塔里木盆地孔雀河地区构造特征.新疆石油地质,26(6)：627-631
汪新文,陈发景.1997.塔北南天山地区震旦-奥陶纪盆-山构造演化及其与油气关系.现代地质,11(3)：313-321
王琪,丁国瑜,乔学军等.2000.天山现今地壳快速缩短与南北地块的相对运动.科学通报,45(14)：1543-1547
王涛,童英,李舢,张建军,史兴俊,李锦轶,韩宝福,洪大卫.2010.阿尔泰造山带
花岗岩时空演变、构造环境及地壳生长意义—以中国阿尔泰为例.岩石矿物学杂
志，6：595-618
王廷印,刘金坤等.1991.塔里木盆地成盆期及裂谷作用初探.见：贾润青主编.中国塔里木盆地北部油气地质研究(第二辑).北京：中国地质大学出版社,p.1-124
王瑜,李锦轶,李文铅.2002.东天山造山带右行剪切变形及构造演化的40Ar-39Ar年代学证据.新疆地质,4(4)：315-319
王招明,田军,申银民,周黎霞,王振宇.2004.塔里木盆地晚泥盆世-早石炭世东河砂岩沉积相.古地理学报,6(3)：289-296
吴昌志,张遵忠,Khin Zaw, Fernando Della-pasque,唐俊华,郑远川,汪传胜,三金柱.2006.东天山觉罗塔格红云滩花岗岩年代学、地球化学及其构造意义.岩石学报,22(5)：1121-1134
吴根耀,马力.2004.“盆”“山”耦合和脱耦：进展,现状和努力方向.大地构造与成矿学,28(1)：81-97
吴国干,夏斌,王核,陈志勇.2003.塔东地区构造变形特征及其分区.新疆地质,21(4)：407-411
吴国干,夏斌,王核,李华启,陈志勇.2004.塔里木东北地区盆山耦合及其对油气成藏的控制.矿物学报,24(4)：218-224
吴国干,李华启,初宝洁,夏斌,王核,卜国民.2002.塔里木盆地东部大地构造演化与油气成藏.大地构造与成矿学.26(3)：229-234
吴文奎,姜常义,杨复,李良辰.1992.南天山榆树沟-铜花山构造混杂体雏议.西安地质学院学报,14(1)：8-13
西安地质调查所.2007.中国天山邻区地质图(1：100万).地质出版社,北京
夏林圻,夏祖春,徐学义,李向民,马中平,王立社.2007.天山岩浆作用.北京：中国大地出版社,p.1-350
夏林圻,夏祖春,徐学义,李向民,马中平.2008.天山及邻区石炭纪-早二叠世裂谷火山岩岩石成因.西北地质,41(4)：1-68
夏林圻,张国伟,夏祖春,徐学义,董云鹏,李向民.2002.天山古生代洋盆开启、闭合时限的岩石学约束-来自震旦纪、石炭纪火山岩的证据.地质通报,21 (2)：55-62
肖文交,韩春明,袁超,陈汉林,孙敏,林寿发,厉子龙,毛启贵,张继恩,孙枢,李继亮.2006.新疆北部石炭纪二叠纪独特的构造·成矿作用：对古亚洲洋构造域南部大地构造演化的制约.岩石学报,22(5)：1062-1076
肖序常,刘训,高锐.2004.新疆南部地壳结构和构造演化.北京：商务印书馆,p.1-270
肖序常,汤耀庆,冯益民,朱宝清,李锦轶,赵民.1992.新疆北部及其邻区大地构造.北京：地质出版社,p.1-169
肖序常,汤耀庆,李锦轶等.1990.试论新疆北部大地构造演化.新疆地质科学,北京：地质出版社,p.47-68
肖学.2007.塔里木盆地孔雀河地区构造特征及演化.成都理工大学学报(自然科学版),34(2)：157-161
校培喜,黄玉华,王育习,王兴安.2006.新疆库鲁克塔格地块东南缘钾长花岗岩的地球化学特征及同位素测年.地质通报,25(6)：725-729
新疆维吾尔自治区地质矿产局.1993.新疆维吾尔自治区区域地质志.北京,地质出版社新疆维吾尔自治区地质矿产局.1993.新疆维吾尔自治区区域地质志.北京,地质出版社
新疆维吾尔自治区区域地层表编写组.1981.西北地区区域地层表：新疆维吾尔自治区分册,北京：地质出版社,p.335-345
许志琴,崔军文.1996.大陆山链变形构造动力学.北京：冶金工业出版社,p.246
许志琴,李思田,张建新,杨经绥,何碧竹,李海兵,林畅松,蔡志慧.塔里木地块与古亚洲/特提斯构造体系的对接.岩石学报,2011,待发表
许志琴,李廷栋,杨经绥,嵇少丞,王宗起,张泽明.2008.大陆动力学的过去,现在和未来—理论与应用.岩石学报,24(7)：1433-1444
许志琴.1984.地壳变形与显微构造.地质出版社：北京,p：1-133
杨经绥等.2011.新疆中天山南缘库米什地区蛇绿岩的锆石U-Pb同位素定年：早古生代洋盆的证据.岩石学报,待发表
杨树德.1994.新疆北部的古板块构造.新疆地质,12(1)：1-8
杨天南,李锦轶,文中田,冯晓飞,王瑜,孙桂华,高立明.2004.中天山地块南北两缘的韧性剪切带.地质学报,78(3)：310-318
杨天南,王小平.2006.新疆库米什早泥盆世侵入岩时代、地球化学及大地构造意义.岩石矿物学杂志,25(5)：401-411
寅海朋.2003.塔里木微板块震旦-寒武系火山岩地球化学及其大地构造意义.西北地质,36(3)：1-6
张传恒,杜维良,刘典波,汪剑,王梦华.2006.塔里木北部周缘前陆盆地早二叠世快速迁移与沉积相突变俯冲板片拆沉的响应.地质学报,80(6)：789-791
张进江.1999.大型走滑带内同构造花岗岩的判别标志.地质科技情报,18(4)：23-26
张良臣,吴乃元.1985.天山地质构造及演化史.新疆地质,3(3)：1-14
张水昌,彭燕,徐志明,邓攀.塔里木盆地海相原油的源岩.1996.塔里木盆地石油地质研究新进展.北京：科学出版社,p.311-320
张鑫,张金亮,覃利娟.2007.塔里木盆地志留系柯坪塔格组砂岩岩石学特征与物源分析.矿物岩石,27(3)：106-115
张兴龙,郑玉洁,倪梁.2004.东天山喀尔力克康古尔塔格组火山岩特征,新疆地质,22(3)：296-299
张志诚,郭召杰,刘树文.1998.新疆库鲁克塔格地区基性岩墙群的岩石地球化学特征、形成时代及其大地构造意义.北京大学国际地质科学学术研讨会论文集,北京：地震出版社,p.124-131
赵德力,肖学,孔凡军,杨云飞,马荣芳,孙潜茹.2005.塔里木盆地孔雀河地区构造变形特征探讨.石油天然气学报,27(6)：681-684
赵孟军,黄第藩.塔里木盆地古生界油源对比.1996.塔里木盆地石油地质研究新进展.北京：科学出版社,p.300-310
周鼎武,苏犁,简平等.2004.南天山榆树沟蛇绿岩构造单元中高压麻粒岩SHRIMP锆石U-Pb年龄及构造意义.科学通报,49(14):1411-1415
周洪瑞,张传恒,王自强,王家生.1998.南天山造山带综合地层学研究.新疆地质,16(4)：291-298
周济元,崔炳芳,陆彦.1999.新疆哈密玉西银矿床特征及成因.矿床地质,18(3)：209-217
周济元,崔炳芳,肖惠良,陈世忠.2008.中国新疆库鲁克塔格-星星峡地区金、银和铜矿地质及预测.北京：地质出版社,p：1-429
周晶,季建清,韩宝福,马芳,龚俊峰,徐芹芹,郭召杰.2008.新疆北部基性岩脉40Ar/39Ar年代学研究.24(5)：997-1010.
周新源,李曰俊,王招明,李宇平,罗俊成,张博.2002.塔里木盆地西北缘乌什南上奥陶统-下志留统沉积构造背景初探.地质科学,37(增刊)：57-63
朱宝清,冯益民,杨军录等.2002.新疆中天山干沟一带蛇绿混杂岩和志留纪前陆盆地的发现及其意义.新疆地质,20(4)：326-330
朱文斌,舒良树,孙岩,郭继春,郭令智,王锋.2004.塔里木北缘晚新生代断裂活动的年代学.矿物学报,24(3)：225-230
朱志澄.1999.构造地质学.中国地质大学出版社：武汉,p：1-261
Allen M B, Windley B F, Zhang C.1994. Cenozoic tectonics in the Urumqi-Korla region of the Chinese Tianshan. Geol Rundsch,83:406-416
Andrsen T.2002. Correction of common lead in U-Pb analyses that do not report 204Pb. Chemical Geology,192:59-79
Bacon G R and Druit T H.1988. Compositional evolution of the zoned talc-alkaline magna chamber of Mount Mazama, Crater Lake, Oregon. Contrib. Mineral. Petrol.,98:224-256
Bhatia M R.1983. Plate tectonics and geochemical composition of sandstones. Journal of Geology,91:611-627
Brookfield M E.2000. Geological development and Phanerozoic crustal accretion in the western segment of the southern Tianshan (Kyrgyzstan, Uzbekistan and Tagikistan). Tectonophysics,328:1-14
Bullen M E, Burbank D W, Garver J I.2001. Late Cenozoic tectonic evolution of the northwestern Tian Shan New age estimates for the initiation of mountain building DSR bulletin.113(12):1544-1559
Burchfiel B C, Royden L H.1991. Tectonics of Asia 50 years after the death of Emile Argand. Eclogae Geol Helv,84:599-629
Busby C J, Ingersoll R V.1995. Tectonics of sedimentary basins.Oxford:Blackwell Science
Chen C, Lu H, Jia D, et al.1999. Closing history of the southern Tianshan oceanic basin, western China:an oblique collisonal orogeny. Tectonophysics,302: 23-40.
Christiansen R L.1984. Yellowstone magmatie evolution; its bearing on understanding large volume explosive volcanism. In Explowive Volcanism; Inception, evolution and hazards. National Academy Press, Washington D C, 84-95
Cloetingh S, Ben Avraham Z, Sassi W, Horvath F.1996. Dynamics of Extensional Basins and inversion Tectonics. Tectonophysics,266:1-523
Cloetingh S, Eldholm O, Larsen B T, Gabrielsen R, Sassi W.1994. Dynamics of Extensional Basin Formation. Tectonophysics,240:1-341
Cloetingh S, Sassi W, Hoevath F.1993. The origin of Sedimentary Basins:Inferences from Quantative Modelling and Basin Analysis. Tectonophysics,226:1-518
Dewey J F, Bird J M.1970. Mountain belts and new global tectonic. Geophys Res,75: 2625-2647
Ernst W G. 2005. Alpine and Pacific styles of Phanerozoic mountain building: subduction zone petrogenesis of continental crust.Tarra Nova,17:165-188
Gao J, Klemd R.2003. Formation of HP-LT rocks and their tectonic implications in the western Tianshan Orogen, NW China:geochemical and age constraints. Lithos,66:1-22
Gao J, Li M S, Xiao X C, Tang Y Q, He G Q.1998. Paleozoic tectonic evolution of the Tianshan orogen, northwestern China. Tectonophysics,287:213-231
Gao J, Long L L, Klemd R, Qian Q et al.2009. Tectonic evolution of the south Tianshan orogen and adjacent regions, NW China:geochemical and age constraints of granitoid rocks. Int. J. Earth Scie. (Geol Rundsch),98:1221-1238
Gao J, He G Q, Li M S, Xiao X C, Tang Y Q, Wang J, Zhao M.1995. The mineralogy,petrology,metamorphic PTDt trajectory and exhumation mechanism of blueschists,south Tianshan, northwestern China. Tectonophysics 250:151 168
Gao J, Klemd R, Qian Q, Zhang X, et al.2011. The collision between the Yili and Tarim blocks of the Southwestern Altaids:Geochemical and age constraints of a leucogranite dike crosscutting the HP-LT metamorphic belt in the Chinese Tianshan Orogen. Tectonophysics. impress.
Grove T L and Donnelly-Nolan M.1986. The evolution of young sillic lavas at Medicine Lake volcano, California:implications for the origin of compositional gaps in calc-alkaline series lavas. Contrub. Mineral. Petol.,92 (2):281-302
Hsu K J, Yao Y, Hao J, Hsu P, Li J andWangO.1994. Origin ofChinese Tianshan by arc-arc collisions. Eclogae GolHelv,87(1):65-292
Hu A Q, Jahn B M, Zhang G X, Chen Y B, Zhang Q F.2000. Crustal Evolution and Phanerozoic Crustal Growth in Northern Xinjiang:Nd Isotopic Evidence. Part Ⅰ: Isotopic Characterization of Basement Rocks. Tectonophysics,15-51
Hu A Q, Rogers G. 1992. Discovery of 3.3 Ga Archean rocks in north Tarim Block of Xinjiang, western China. Chinese Science Bulletin,37 (18):1546-1549
Huton D H W, Reavy R J.1992. Strike-slip tectonics and granite petrogenesis.Tectonics,11:960-967
Jahn B m, Windley B, Natalin, B, et al.2004. Phanerozoic continental growth in Central Asia. Journal of Asian Earth Sciences,23:599-603
Koppers A A P.2002. Software for 39Ar/40Ar age calculations. Computers and Geosciencs,28:605-619
Kroner A., Windley B F, Badarch G, Tomurtogoo O, Hegner E, Jahn B M, Gruschka S, Khain E V, Demoux A, Wingate M T D.2007. Accretionary growth and crustformation in the central Asian Orogenic Belt and comparison with the Arabian-Nubian shield. In:Hatcher Jr., R.D., Carlson, M.P., McBride, J.H., Martinez Catalan, J.R. (Eds.),4-D Framework of Continental Crust: Geological Society of America Memoir,200, p.181-209.10.1130/2007.1200(11).
Laurent-Charvet S, Charvet J, Shu L S, Ma R S and Lu H E.2002. Paleozoic late collisional strikeslip dcformations in Tianshan and Altay, Eastern Xinjiang, NW China. Terra Nova,14:245-256
Laurent-Charvet S, Charvet J, ShuLS, et al.2002. Ductile strike-slip shear zones in Eastern Xinjiang, NW China:ALate Palaeozoic late collisional intracontinental adjustment. Terra Nova,14 (4):249-256
Laurent-Charvet S, MonieP, Charvet J, et al.2003. Late-Paleozoic strike-slip shear zones in northeastern Xinjiang (NW China):new structural and geochronological data. Tectonics,22 (2):1009-1032
Le Bas M J, Le Maitre R W, Streckeisen A, et al.1986. A chemical classification of volcanic rocks based on the total alkali-silica diagram. Journal of Petrology,27: 745-750
Li Y J, Sun L D, Wu H R, Zhang G Y, Wang G L, Huang Z B.2005. Permo Carboniferous radiolarians from the Wupata' erkan group, Western South Tianshan, Xinjiang, China. Acta Geologica Sinica,79 (1):16-23
Li Y J, Wang Z M, Wu H R, Huang Z B, Tan Z J, Luo J C. 2002. Discovery of radiolarian fossils from the Aiketik group at the western end of the South Tianshan Mountains of China and its implications. Acta Geologica Sinica, 76 (2): 146-154
Liu Y L, Zhang Z C, Guo Z J, Huang B L, Mu Z G. 1999. K Ar isochron dating of Kuluktag mafic dykes, Xinjiang autonomous region, and discussion on some related questions. Geological Journal of China Universities,5 (1):55-58
Liu Y S, Hu Z C, Gao S, Gunther D, Xu J, Gao C, Chen H.2008. In situ analysis of major and trace elements of anhydrous minerals by LA-ICP-MS without applying an internal standard. Chemical Geology,257:34-43
Liu Y, Hao S G. 2006. Evolutionary significance of pylentonemid radiolarians and their Late Devonian species from southwestern Tianshan, China. Acta Geologica Sinica,80 (5):647-655
Liu Y.2001. Early Carboniferous radiolarian fauna from Heiyingshan South of the Tianshan Mountains and its geotectonic significance. Acta Geologica Sinica,75 (1):101-108
Luddwig K R.1991. Isoplot-aplotting and regression program for radiogenic-isotope data. U S Geological Survey Open-file report,39:91-445
Ludwig K R.1991. ISOPLOT:A Plotting and Regression Program for Radiogenic isotope Data. US Geological Survey Open File Report, p.1-39
Mossakovsky A A, Ruzhentsev S V, Samygin S G, Kheraskova T N.1993. The Central Asian fold belt:geodynamic evolution and formation history. Geotectonics,26: 455-473
Price R A, Mountjoy E W.1971. Geologic structure of the Canadian Rocky Mountains between Bow and Athabasca Rivers a progress report. In:Wheeler JO (ed). Structure of the southern Canadian Cordillera:GeologicalAssociation ofCanada SpecialPaper,6:7-26
Reavy R J.1989. Structural controls on metamorphism and syntectonic magmatism: the Portuguese Hercynian collision belt. Journal of Geology Society London,146: 649-657
Ring U, Kroner A, Layer P, et al.1999. Deformed A-type granites in norther Malawi, east-central Africa:pre-or syntectonic? Jounal of the Geological Society, London,156:695-714
Roser B P, Korsch R J.1986. Determination of tectonic setting sandstone-mudstone suites using SiO2 content and K2O/Na2O ratio. Journal of Geology,94 (5): 635-650
Rurn J P, Cobbold P R.1980. Strain heating and thermal softening incontinental shear zones:a review.Journal of Structural Geology,2:149-158
Schumm S A, Dumont J F.2000. Active tectonics and alluvial rivers. Cambridge: Cambridge University Press, p.1-276
Sebastien Laurent-Charvet, Jacques Charvet, Liangshu Shu, Ruishi Ma, Huafu Lu. 2002. Palaeozoic late collisional strike-slip deformations in Tianshan and Altay, Eastern Xinjiang, NW China. Terra Nova,14 (4):249-256.
Sebastien Laurent-Charvet, Jacques Charvet, Patrick Monie, Liangshu Shu. Late Paleozoic strike-slip shear zones in eastern central Asia (NW China):New structural and geochronological data. Tectonics, doi:10.1029/2001TC901047.
Sengor A M C, Natal'in B A., Burtman V S.1993. Evolution of the Altaid tectonic collage andm Palaeozoic crustal growth in Eurasia. Nature,364:299-307
Sengor A M C, Natal'in B A.1996. Paleotectonics of Asia: fragments of a synthesis.In: Yin A, et al., eds. The Tectonic Evolution of Asia.Cambridge:Cambridge University Press, p.486-640
Sengor A M C.1990. Plate tectonics and orogenic research after 25 years:a Tethya perspective.Earth Science Reviewe,27:1-201
Sengor A M C.1992.板块构造学与造山运动-特提斯例析.丁晓翻译,上海.复旦大学出版社,p.1-182
Sengor A M C., Natalin B.1996. Turkic-type orogeny and its role in the making of the continental crust. Annual Reviews of Earth and Planetary Sciences,24: 263-337
Shu L S, Charvet J, Guo L Z, et al.1999. Laurent-Charvet Sebastien. A large-scale Palaeozoic dextral ductile strike-slip zone:the Aqqikkudug-Weiya zone along the northern margin of the Central Tianshan belt, Xinjiang, NW China. Acta Geol. Sinica,73 (2):148-162
Shu L S, Charvet J, Lu H F, et al.2002. Paleozoic accretion-collision events and kinematicsof ductile deformation in the central-southern Tianshan Belt, China. Acta Geol. Sinica,76 (3):308-323
Shu L S, Charvet J, Ma R S.1998. Study of a large scale Paleozoic dextral strike-slip ductile shear zone along the northern margin of the central Tianshan, Xinjiang. Xinjiang Geology,16 (4):326-336
Sun S S, Mcdonough W F.1989. Chemical and isotopic systematics of oceanic basalts: implications for mantle composition and Processes.Saunders A D, Norry M J. Magmatism in the Ocean Basins. London:Geol. Soc. Spec. Pub.,42:313-45
Tapponnier P, Peltzer G, Armijo R.1986. On the mechanics of the collision between India and Asia. Geol Soc Spec Publ,19:115-157
Wang X W, Chen F J.1997. Sinian-Ordovician tectonic evolution of north Tarim and south Tianshan region and its relation to oil and gas. Geoscience-Journal of Graduate School, China University of Geoscience,11 (3):313-321
Willson W.1989. Igneous petrogenesis. Unwin Hyman, London, p.327-373
Wilson J T.1990. On the building and classification of Mountains. J Geophys Res,95: 6611-6628
Windley B F, Alexeiev D, Xiao W, Kroner A, Badarch G 2007. Tectonic models for accretion of the Central Asian Orogenic belt. Journal of the Geological Society, London,164:31-47
Windley BF, Allen MB, Zhang C, Zhao Z, Wang Q.1990. Paleozoic accretion and Cenozoic redeformation of the Chinese Tien Shan range,central Asia.Geology,18: 128-131
Xiao W J, Han C M, Yuan C, Sun M, Lin S F, Chen H L, Li Z L, Li J L, Sun S.2008. Middle Cambrian to Permian subduction-related accretionary orogenesis of Northern Xinjiang, NW China:Implications for the tectonic evolution of central Asia. Journal of Asian Earth Sciences,32:102-117
Xiao W J, Huang B C, Han C M, Sun S, Li J L.2010. A review of the western part of the Altaids:A key to understanding the architecture of accretionary orogens. Gondwana Research,18 (2-3):253-273
Xiao W J, Zhang L C, Qin K Z, Sun S, Li J L.2004. Paleozoic accretionary and collisional tectonics of the eastern Tianshan (China):Implications for the continental growth of Central Asia. American Journal of Science,304:370-395
Xu B, Xiao S H, Zou H B, Chen Y, et al.2009. SHRIMP zircon U-Pb age constraints on Neoproterozoic Quruqtagh diamictites in NW China,168:247-258
Xu B, Zhang H, Yao H, Li Y.2003. Gisotopeeom sitionand signifieanee of the Sinianon theTarim Plate. Chinese Science Bullitin,48:385-389
Yang T N, Wang Y, Li J Y, Sun G H.2007. Vertical and horizontal strain partitioning of the Central Tianshan (NW China):Evidence from structures and 40Ar/39Ar geochronology. Journal of Structural Geology,29:1605-1621
Yin A, Nie S. Craig P and Harrison T M.1998. Late Cenozoic tectonic evolution of the South Chinese Tian Shan. Tectonics,17(1):1-27
Zhang L, Ai Y L, Li X P, Rubatto D, Song B, Williams S, Song S G, Ellis D, Liou J G.2007. Triassic collision of western Tianshan orogenic belt, China: Evidence from SHRIMP U-Pb dating of zircon from HP/UHP eclogitic rocks. Lithos,96:266-280
蔡东升,卢华复.1996.南天山蛇绿混杂岩和中天山南缘糜棱岩的40Ar/39Ar年龄及其大地构.地质科学,31(4)：384-390
车自成,刘洪福,刘良等.1994.中天山造山带的形成与演化.北京：地质出版社,p.1-142
陈汉林,杨树锋,董传万,贾承造,魏国齐,汪振国.1997.塔里木盆地二叠纪基性岩带的确定及大地构造意义.地球化学,26(6)：77-86
陈文,孙枢,张彦等.2005.新疆东天山秋格明塔什-黄山韧性剪切带40Ar/39Ar年代学研究.地质学报,79(6)：790-804
成守德,王元龙.1998.新疆大地构造演化基本特征.新疆地质,16(2)：97-107
程日辉,王璞,孙晓猛,白云风.2006.库鲁克塔格地区奥陶系层序地层与海平面变化.大地构造与成矿学,30(3)：283-293
邓松涛,郭召杰,张志诚,廖国辉.2006.南天山中段桑树园子韧性剪切带的形成时限及其构造意义.中国地质,33(3)：641-647
邓兴梁,舒良树,朱文斌,马东升,王博.2008.新疆兴地断裂带前寒武纪构造—岩浆—变形作用特征及其年龄.岩石学报,24(12)：2800-2808
地质部新疆维吾尔自治区地质局.1965.1：20万辛格尔幅地质图说明书.乌鲁木齐：新疆印刷厂
丁振举,姚书振,周宗桂等.2003.碧口群不同岩片火山岩微量元素组成差异与古构造意义,地球科学-中国地质大学学报,20(2)：167-172
董云鹏,王润三,周鼎武.2001.南天山北缘榆树沟变质基性超基性岩的地球化学及其成因机制.地球化学,30(6)：559-568
董云鹏,张国伟,周鼎武,罗金海,张成立,夏林圻,徐学义,李向民.2005.中天山北缘冰达坂蛇绿混杂岩的厘定及其构造意义.中国科学D辑：地球科学,35(6)：552-560
范璞,马宝林.1990.塔里木油气地质总论.北京：科学出版社,p.1-258
冯益民,朱宝清,杨军录等.2002.东天山大地构造及演化-1：50万东天山大地构造图简要说明.新疆地质,20(4)：309-314
高俊,龙灵利,钱青,黄德志,苏文.2006.南天山：晚古生代还是三叠纪碰撞造山带.岩石学报,22(5)：1049-1061
高俊,钱青,龙灵利,张喜,李继磊,苏文.2009.西天山的增生造山过程.28(12)：1804-1816
高俊,肖序常,汤耀庆,赵民,王军,吴汉泉.1993.南天山库米什蓝片岩的发现及其大地构造意义.中国区域地质,4：344-347
高锐,肖序常,高弘.2002.西昆仑-塔里木-天山岩石圈深地震探测综述.地质通报,21(1)：11-18
高振家,陈晋镳,陆松年,彭昌文等.1993.新疆北部前寒武系.前寒武纪地质第六号.北京：地质出版社
高振家,王务严,彭昌文等.1985.新疆震旦系(新疆地层总结之一).乌鲁木齐：新疆人民出版社,p.35-73
郭令智,施央申,卢华复.1992.印藏碰撞的两种远距离构造效应.现代地质学研究文集(上).南京：南京大学出版社,p.81-91
郭召杰,韩宝福,张志诚,邓松涛,刘畅.2007.中天山东段古生代淡色花岗岩的发现及其构造意义.岩石学报,23(8)：1841-1846
郭召杰,张志诚,廖国辉.2002.天山东段隆升过程的裂变径迹年龄证据及构造意义.新疆地质,20(4)：331-334
郭召杰,马瑞士,郭令智,施央申.1993.新疆东部三条蛇绿混杂带的比较研究.地质论评,39(3)：236-247
韩宝福,何国琦,吴泰然,李惠民.2004.天山早古生代花岗岩锆石U-Pb定年、岩石地球化学特征及其大地构造意义.新疆地质,22(1)：4-11
何登发,李德生.1996.塔里木盆地构造演化与油气聚集.北京：地质出版社,p.1-173
何国琦,李茂松,韩宝福.2001.中国西南天山及邻区大地构造研究.新疆地质,19(1)：7-11
何国琦,李茂松,刘德权,唐延龄,周汝洪.1994.中国新疆古生代地壳演化及成矿.乌鲁木齐：新疆人民出版社；香港：香港文化教育出版社,p.1-437
胡霭琴,王中刚,涂光炽等.1997.新疆北部地质演化及成矿规律.北京：科学出版社,p.9-35
胡霭琴,韦刚建.2006.塔里木盆地北缘新太古代辛格尔灰色片麻岩形成时代问题,地质学报,80(1)：126-133
胡霭琴,韦刚健,张积斌,邓文峰,陈林丽.2007.天山东段天湖东片麻状花岗岩的锆石SHRIMP U-Pb年龄和构造演化意义.岩石学,23(8)：1795-1802
胡霭琴,张国新,陈义兵等.2001.新疆大陆基底分区模式和主要地质事件的划分.新疆地质,19(1)：12-19
胡霭琴,张国新,张前锋,陈义兵.1999.天山造山带基底时代和地壳增生的Nd同位素制约.中国科学D辑：地球科学,29(2)：104-112
胡霭琴,张国新等.1995.新疆北部主要地质事件同位素年表,地球化学,24(1)：20-31
胡受奚,郭继吞,顾连兴等.1990.加里东造山带在东天山(E85°-90°),构造格架中的重要地位及其地质特征.新疆地质科学,地质出版社,32-46
黄汲清.1990.新疆及邻区板块开合构造及手风琴式运动.新疆地质科学,(1)：3-16
贾承造,姚慧君,魏国齐.1995.塔里木盆地板块构造演化和主要构造单元地质构造特征.北京：石油工业出版社,p.45-280
姜常义,姜寒冰,叶书锋,夏明哲,逯东霞.2005.新疆库鲁克塔格地区二叠纪岩脉群岩石地球化学特征,Nd、Sr、Pb同位素组成与岩石成因.地质学报,79(6)：823-833
姜常义,吴文奎,李良辰.2001.南天山东段显生宙构造演化.北京：地质出版社,1-160
姜常义,杨复,吴文奎,李良辰.1990.库米什地区火山岩岩石地球化学特征及大地构造环境,西安地质学院学报,12(1)：1-8
姜常义等,2001.天山地区新元古代-早寒武世火山岩地球化学和岩石成因.岩石矿物学杂志,25(5)：412-422
金文正,汤良杰,王清华,余一欣,万桂梅,杨文静,彭更新,雷刚林.2007.库车前陆盆地东秋里塔格构造带构造分段特征.大地构造与成矿学,31(3)：300-307
康玉柱.1993.塔里木盆地形成演化及构造特征与油气关系.新疆地质,11(2)：95-107
李春昱,王荃.1983.我国北部边陲及邻区的古板块构造与欧亚大陆的形成.见中国北方板块构造文集(1).北京：地质出版社
李海兵,杨经绥,许志琴,孙知明等.2006.阿尔金断裂带对青藏高原北部生长、隆升的制约.地学前缘,13(4)：59-79
李华芹,陈富文,蔡红,刘后群.1999.新疆东部马庄山金矿成矿作用同位素年代学研究.地质科学,34(2)：251-256
李继亮,孙枢,郝杰,陈海泓,侯泉林,肖文交,吴继敏.1999.碰撞造山带的碰撞事件时限的确定.岩石学报,15(2)：315-320
李继亮.1989.准噶尔残留弧后盆地与中天山造山带的大地构造关系.沉积学报,7(增刊)：53-61
李锦轶,何国琦,徐新等.2006.新疆北部及邻区地壳构造格架及其形成过程的初步探讨.地质学报,80(1)：148-168
李锦轶,王克卓,李亚萍,孙桂华,褚春华,李丽群,朱志新.2006.天山山脉地貌特征、地壳组成与地质演化.地质通报,25(8)：895-909
李锦轶.2004.新疆东部新元古代晚期至古生代的构造格局与构造演化.地质论评,50(3)：304-322
李伍平,王涛,李金宝,康旭,于福生,韩庆军,马忠平.2001.东天山红柳河地区海西期花岗岩的岩石学、地球化学及其构造环境.地质论评,47(4)：368-376
李向东,肖文交,周宗良.2004.南天山南缘晚泥盆世构造事件的40Ar/39Ar定年证据及其意义.岩石学报,20(3)：691-696
李向民,夏林圻,夏祖春,徐学义,马中平.2006.天山地区新元古代-早寒武世火山岩地球化学和岩石成因.岩石矿物学杂志,25(5)：412-422
李曰俊,孙龙德,吴浩若,张光亚,王国林,黄智斌.2004.南天山西段库尔干地区三叠纪砾岩的硅岩砾石中发现放射虫化石.地质科学,39(2)：153-158
李曰俊,王招明,周黎霞.2000.塔里木盆地西北部乌什地区构造单元划分和盆山耦合关系.见：王福同主编,第四届天山地质矿产资源学术讨论会论文集.乌鲁木齐：新疆人民出版社,p.27-30
李曰俊,杨海军,赵岩,罗俊成,郑多明,刘亚雷.2009.南天山区域大地构造与演化.大地构造与成矿学,33(1)：94-104
刘畅,赵泽辉,郭召杰.2006.甘肃北山地区煌斑岩的年代学和地球化学及其壳幔作用过程讨论.岩石学报,22(5)：1294-1306
刘训,吴绍祖,傅德荣,姚建新,丁孝忠,王永.1997.塔里木板块周缘的沉积-构造演化.新疆：新疆科技卫生出版社,p.1-256
刘玉琳,张志诚,郭召杰,黄宝玲,穆志国.1999.库鲁克塔格基性岩墙群K-Ar等时年龄测定及其有关问题讨论.高校地质学报,5(1)：55-58
卢德源,李秋生,高锐等.2000.横跨天山的人工爆炸地震剖面.科学通报,45(9)：982-988
卢华复,贾东,蔡东升,吴世敏.1996.塔里木与西天山板块构造演化.见：童晓克,梁狄刚,贾承造主编.塔里木盆地石油地质研究新进展.北京：科学出版社,p.235-245
卢华复,王胜利,贾东,王良书,刘绍文.2005.塔里木盆地与天山山脉晚新生代盆山耦合机制,高校地质学报,11(4)：493-503
卢华复,王胜利,罗俊成等.2006.塔里木盆地东部断裂系统及其构造演化.石油与天然气地质,27(4)：433-441
陆松年,李怀坤,陈志宏.2003.塔里木与扬子新元古代热构造事件特征、序列和时代—扬子与塔里木连接(ABCDEF)假设.地学前缘,10(4)：321-326
陆松年等编著.2006.中国前寒武纪重大地质问题研究：中国西部前寒武纪重大地质事件群及其全球构造意义.地质出版社.
罗新荣,石福品,樊卫东,罗新涛.2007.新疆库鲁克塔格新元古代花岗岩年龄和地球化学.资源调查与环境,28(4)：235-241
马华东,贺卫东,涂其军,陈静,曹福根,任燕.2008.新疆东天山地区塔水河韧性剪切带特征.大地构造与成矿学,32(1)：1-10
马瑞士,王赐银,叶尚夫等.1993.东天山构造格架及地壳演化.南京：南京大学出版社,p.1-225
马杏垣.2004.解析构造学.北京：地质出版社,p.1-463
潘家伟,李海兵,Jerome Van Der Woerd,孙知明.2007.西昆仑山前冲断带晚新生代构造地貌特征.地质通报,26(10)：1368-1379
任战利,肖晖,韩伟,梁宇,卿颖,腾志宏,史政.2009.孔雀河斜坡与库鲁克隆起构造-热演化史研究.39(3)：510-516
石玉若,刘敦一,张旗,简平,张福勤,苗来成.2006.中天山干沟一带花岗质岩类SHRIMP年代学及其构造意义.科学通报,51(22)：2665-2672
舒良树,郭召杰,朱文斌,卢华复,王博.2004.天山地区碰撞后构造与盆山演化.高校地质学报,10(3)：393-404
舒良树,卢华复,印栋豪,王博.2003.中、南天山古生代增生-碰撞事件和变形运动学研究.南京大学学报(自然科学版),39(1)：17-30
舒良树,王博,朱文斌.2007.南天山蛇绿混杂岩中放射虫化石的时代及其构造意义.地质学报,81(9)：1161-1168
舒良树,夏飞雅克,马瑞士.1998.中天山北缘大型右旋走滑韧剪带研究.新疆地质,16(4)：326-336
舒良树,朱文斌,王博,Faure M, Charvel J, Cluzel D.2005.新疆博格达南缘后碰撞期陆内裂谷和水下滑塌构造.岩石学报,21(1)：25-36
舒良树和卢华复.2003.中国中南天山造山带东段古生代增生-碰撞事件和韧性变形的运动学.南京大学学报(自然科学),39(1)：17-31
孙晓猛,王璞瑶,刘鹏举,郝福江.2006.兴地断裂构造特征及其演化历史.新疆地质,24(4)：348-352
汤良杰.1997.略论塔里木古生代盆地演化.现代地质,11(1)：14-20
汤耀庆,高俊,赵民,李锦轶,王军.1995.西南天山蛇绿岩和蓝片岩.北京：地质出版社,p.1-133
唐俊华,顾连兴,张遵忠,吴昌志等.2007.东天山咸水泉片麻状花岗岩特征、年龄及成因.23(8)：1803-1820
唐俊华,顾连兴,郑远川,方同辉,张遵忠,高军辉,王福田,汪传胜,张光辉.2006.东天山卡拉塔格钠质火山岩岩石学、地球化学及成因.岩石学报,2(5)：1150-1166
田纳新,程喆,陈文礼,林学庆.2008.塔里木盆地孔雀河地区构造变形特征及其控油气作用.石油实验地质.30(3)：236-241
田纳新,于明德,涂志民,马玉春.2005.塔里木盆地孔雀河地区构造特征.新疆石油地质,26(6)：627-631
汪新文,陈发景.1997.塔北南天山地区震旦-奥陶纪盆-山构造演化及其与油气关系.现代地质,11(3)：313-321
王琪,丁国瑜,乔学军等.2000.天山现今地壳快速缩短与南北地块的相对运动.科学通报,45(14)：1543-1547
王涛,童英,李舢,张建军,史兴俊,李锦轶,韩宝福,洪大卫.2010.阿尔泰造山带
花岗岩时空演变、构造环境及地壳生长意义—以中国阿尔泰为例.岩石矿物学杂
志，6：595-618
王廷印,刘金坤等.1991.塔里木盆地成盆期及裂谷作用初探.见：贾润青主编.中国塔里木盆地北部油气地质研究(第二辑).北京：中国地质大学出版社,p.1-124
王瑜,李锦轶,李文铅.2002.东天山造山带右行剪切变形及构造演化的40Ar-39Ar年代学证据.新疆地质,4(4)：315-319
王招明,田军,申银民,周黎霞,王振宇.2004.塔里木盆地晚泥盆世-早石炭世东河砂岩沉积相.古地理学报,6(3)：289-296
吴昌志,张遵忠,Khin Zaw, Fernando Della-pasque,唐俊华,郑远川,汪传胜,三金柱.2006.东天山觉罗塔格红云滩花岗岩年代学、地球化学及其构造意义.岩石学报,22(5)：1121-1134
吴根耀,马力.2004.“盆”“山”耦合和脱耦：进展,现状和努力方向.大地构造与成矿学,28(1)：81-97
吴国干,夏斌,王核,陈志勇.2003.塔东地区构造变形特征及其分区.新疆地质,21(4)：407-411
吴国干,夏斌,王核,李华启,陈志勇.2004.塔里木东北地区盆山耦合及其对油气成藏的控制.矿物学报,24(4)：218-224
吴国干,李华启,初宝洁,夏斌,王核,卜国民.2002.塔里木盆地东部大地构造演化与油气成藏.大地构造与成矿学.26(3)：229-234
吴文奎,姜常义,杨复,李良辰.1992.南天山榆树沟-铜花山构造混杂体雏议.西安地质学院学报,14(1)：8-13
西安地质调查所.2007.中国天山邻区地质图(1：100万).地质出版社,北京
夏林圻,夏祖春,徐学义,李向民,马中平,王立社.2007.天山岩浆作用.北京：中国大地出版社,p.1-350
夏林圻,夏祖春,徐学义,李向民,马中平.2008.天山及邻区石炭纪-早二叠世裂谷火山岩岩石成因.西北地质,41(4)：1-68
夏林圻,张国伟,夏祖春,徐学义,董云鹏,李向民.2002.天山古生代洋盆开启、闭合时限的岩石学约束-来自震旦纪、石炭纪火山岩的证据.地质通报,21 (2)：55-62
肖文交,韩春明,袁超,陈汉林,孙敏,林寿发,厉子龙,毛启贵,张继恩,孙枢,李继亮.2006.新疆北部石炭纪二叠纪独特的构造·成矿作用：对古亚洲洋构造域南部大地构造演化的制约.岩石学报,22(5)：1062-1076
肖序常,刘训,高锐.2004.新疆南部地壳结构和构造演化.北京：商务印书馆,p.1-270
肖序常,汤耀庆,冯益民,朱宝清,李锦轶,赵民.1992.新疆北部及其邻区大地构造.北京：地质出版社,p.1-169
肖序常,汤耀庆,李锦轶等.1990.试论新疆北部大地构造演化.新疆地质科学,北京：地质出版社,p.47-68
肖学.2007.塔里木盆地孔雀河地区构造特征及演化.成都理工大学学报(自然科学版),34(2)：157-161
校培喜,黄玉华,王育习,王兴安.2006.新疆库鲁克塔格地块东南缘钾长花岗岩的地球化学特征及同位素测年.地质通报,25(6)：725-729
新疆维吾尔自治区地质矿产局.1993.新疆维吾尔自治区区域地质志.北京,地质出版社新疆维吾尔自治区地质矿产局.1993.新疆维吾尔自治区区域地质志.北京,地质出版社
新疆维吾尔自治区区域地层表编写组.1981.西北地区区域地层表：新疆维吾尔自治区分册,北京：地质出版社,p.335-345
许志琴,崔军文.1996.大陆山链变形构造动力学.北京：冶金工业出版社,p.246
许志琴,李思田,张建新,杨经绥,何碧竹,李海兵,林畅松,蔡志慧.塔里木地块与古亚洲/特提斯构造体系的对接.岩石学报,2011,待发表
许志琴,李廷栋,杨经绥,嵇少丞,王宗起,张泽明.2008.大陆动力学的过去,现在和未来—理论与应用.岩石学报,24(7)：1433-1444
许志琴.1984.地壳变形与显微构造.地质出版社：北京,p：1-133
杨经绥等.2011.新疆中天山南缘库米什地区蛇绿岩的锆石U-Pb同位素定年：早古生代洋盆的证据.岩石学报,待发表
杨树德.1994.新疆北部的古板块构造.新疆地质,12(1)：1-8
杨天南,李锦轶,文中田,冯晓飞,王瑜,孙桂华,高立明.2004.中天山地块南北两缘的韧性剪切带.地质学报,78(3)：310-318
杨天南,王小平.2006.新疆库米什早泥盆世侵入岩时代、地球化学及大地构造意义.岩石矿物学杂志,25(5)：401-411
寅海朋.2003.塔里木微板块震旦-寒武系火山岩地球化学及其大地构造意义.西北地质,36(3)：1-6
张传恒,杜维良,刘典波,汪剑,王梦华.2006.塔里木北部周缘前陆盆地早二叠世快速迁移与沉积相突变俯冲板片拆沉的响应.地质学报,80(6)：789-791
张进江.1999.大型走滑带内同构造花岗岩的判别标志.地质科技情报,18(4)：23-26
张良臣,吴乃元.1985.天山地质构造及演化史.新疆地质,3(3)：1-14
张水昌,彭燕,徐志明,邓攀.塔里木盆地海相原油的源岩.1996.塔里木盆地石油地质研究新进展.北京：科学出版社,p.311-320
张鑫,张金亮,覃利娟.2007.塔里木盆地志留系柯坪塔格组砂岩岩石学特征与物源分析.矿物岩石,27(3)：106-115
张兴龙,郑玉洁,倪梁.2004.东天山喀尔力克康古尔塔格组火山岩特征,新疆地质,22(3)：296-299
张志诚,郭召杰,刘树文.1998.新疆库鲁克塔格地区基性岩墙群的岩石地球化学特征、形成时代及其大地构造意义.北京大学国际地质科学学术研讨会论文集,北京：地震出版社,p.124-131
赵德力,肖学,孔凡军,杨云飞,马荣芳,孙潜茹.2005.塔里木盆地孔雀河地区构造变形特征探讨.石油天然气学报,27(6)：681-684
赵孟军,黄第藩.塔里木盆地古生界油源对比.1996.塔里木盆地石油地质研究新进展.北京：科学出版社,p.300-310
周鼎武,苏犁,简平等.2004.南天山榆树沟蛇绿岩构造单元中高压麻粒岩SHRIMP锆石U-Pb年龄及构造意义.科学通报,49(14):1411-1415
周洪瑞,张传恒,王自强,王家生.1998.南天山造山带综合地层学研究.新疆地质,16(4)：291-298
周济元,崔炳芳,陆彦.1999.新疆哈密玉西银矿床特征及成因.矿床地质,18(3)：209-217
周济元,崔炳芳,肖惠良,陈世忠.2008.中国新疆库鲁克塔格-星星峡地区金、银和铜矿地质及预测.北京：地质出版社,p：1-429
周晶,季建清,韩宝福,马芳,龚俊峰,徐芹芹,郭召杰.2008.新疆北部基性岩脉40Ar/39Ar年代学研究.24(5)：997-1010.
周新源,李曰俊,王招明,李宇平,罗俊成,张博.2002.塔里木盆地西北缘乌什南上奥陶统-下志留统沉积构造背景初探.地质科学,37(增刊)：57-63
朱宝清,冯益民,杨军录等.2002.新疆中天山干沟一带蛇绿混杂岩和志留纪前陆盆地的发现及其意义.新疆地质,20(4)：326-330
朱文斌,舒良树,孙岩,郭继春,郭令智,王锋.2004.塔里木北缘晚新生代断裂活动的年代学.矿物学报,24(3)：225-230
朱志澄.1999.构造地质学.中国地质大学出版社：武汉,p：1-261
© 2004-2018 中国地质图书馆版权所有 京ICP备05064691号 京公网安备11010802017129号 地址：北京市海淀区学院路29号 邮编：100083 电话：办公室：(+86 10)66554848；文献借阅、咨询服务、科技查新：66554700 |