大别造山带碰撞后构造热/岩浆演化过程
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摘要
本论文借助于热年代学、构造解析与地球化学等手段，对大别造山带晚后期(晚侏罗世以来)构造热／岩浆过程进行研究：
(1)热年代学分析表明：140～85Ma大别造山带进入热窿伸展时期，由此引发广泛基底熔融、火山剧烈喷溢与盆地断陷作甩，这次热窿事件包括强热伸展阶段(140～105Ma)和晚期衰退阶段(105～85Ma)。在强热伸展阶段，热窿作用集中在大别／红安地块，并以大别地块最为强烈。大别热窿鱼括麻城-岳西热轴、穹核组合以及外围下滑系统，热轴平行造山带延向展布，北淮阳与(超)高压单元构成下滑系统，岳西、罗田热窿核占据麻城-岳西热轴东、西两端，它们最终成型时代不一致。热窿伸展进程伴随着大别强热中心沿着热伸展轴迁移摆动，这说明造山根拆沉过程以间歇性、迁移性、规模性与区域差异性为特征。在伸展退阶段，大别山仍显现穹状轮廓，但伸展强度与岩浆作用显著减弱。
(2)构造解析表明：在现今剥露面内，大别山以伸热窿格局(140～85Ma)为主导，包括热窿核→剥离断裂带→下滑系统配置单元，热窿作用在商麻断裂两侧差异性显著。红安区热窿包括福田河／卡房窿核与红安群／北淮阳下滑系统，平天畈、熊店-浒湾、丰店-七里坪以及大悟-浠水等断裂构成滑脱带，(低)角闪岩相热伸展集中在窿核处，在下滑系统中发育绿片岩相伸展。大别区热窿由罗田／岳西窿核与北淮阳／南大别(超)高压下滑单元构成，其间(内)存在英山-新洲、磨子潭-晓天、太湖-浠水等滑脱带。大别热窿由中深到浅层次剥露过程对应着角闪岩相、低角闪岩相到绿片岩相退变质序列。
(3)低温年代学分析表明：90Ma±造山带热窿构造最终被热断陷交切短轴热隆格局所取代，这种构造格局可一直延续到K～E(90～32Ma)时期(后期出现热分异与穹窿组合)，其形成机制应该与西太平洋域汇聚特性引发区域差异推隆作用相关，这种推隆过程对于大别山现代地形建立有重要贡献。大别山AFT模拟热史还记录其它三次热构造事件：古新世(58～65Ma)热事件在造山带南北侧近边界断裂处影响显著，并在北淮阳与北缘盆地最为强烈；渐新世(30～34Ma)热事件广泛影响到整个造山带与北侧盆地；中新世(13～20Ma)热扰动集中在大别、红安两地块，而在北淮阳与合肥盆地相当微弱；推测这些热构造事件应该与西部碰撞域、东部汇聚域以及南海盆地扩张／关闭远场响应有关。
(4)地球化学分析表明，大别造山带构造／岩浆事件(中生代以来)包括六期，汇聚“岛弧”事件(〉240Ma)、板块“断离”事件(210Ma±)、挤压“加厚”事件(早～中侏罗世)、造山带“去根”事件(早白垩世)、远场“扩张”事件(85～53Ma)与“地幔羽”事件(渐新世以来)。大别山热窿伸展与造山带“去根”作用密切相关，岩浆显示TiO_2、Nb、P_2O_5亏损、Ba、La、K_2O富集特点，岩浆源区显著亲合于EMI端元和下地壳。进入晚白垩世～古新世，由于受西太平洋汇聚域弧后扩张作用制约，火山岩钾质含量减少，岩浆源区位于BSE与EMI之间。渐新世以来，地幔羽事件以岩浆显著亲合PREMA幔源和洋岛玄武岩为标志。
(5)对比邻区表明：①晚侏罗世～早白垩世，大别山源源(EMI)岩浆形成与造山根拆沉熔入地幔再循环有关，东南区幔源(EMI与EMII过渡)岩浆特性应该与洋壳俯冲沉积物加入、西太平洋汇聚域弧后扩张、以及大陆地幔上隆作用相联系，而下扬子岩浆兼有“拆沉”混合幔源(大别山)与弧后扩张幔源(东南区)过渡性质。大别造山带演化与东部大陆边缘显现构造制约关系，造山带“去根”作用属于造山晚后期构造与西太平洋域弧后扩张叠置产物。②晚白垩世～古新世，大别山与下扬子、东南区火山岩趋向洋岛玄武岩组成，同位素向着εNd增加、~(87)sr~(86)Sr减少方向演化，地幔源区与BSE端元大致亲合。这一时期，我国东部火山作用逐渐趋于统一幔源与统一扩张环境，而大别山晚后造山期演化渐趋于终结。③渐新世以来，统一构造环境与同一幔源区控制着我国东部火山作用，该时期火山岩显著亲合于PREMA幔源和洋岛玄武岩组成，橄榄岩包体指示深部存在PREMA地幔端元，这种特性应该与西太平洋域弧后扩张、地幔羽作用密切相关。
(6)构造剥离分析表明：大别造山带具有双侧造山特点，(超)高压单元与灰色片麻岩之间为热窿核与下滑系统配置关系，南北大别界限可能不存在。麻城-岳西热轴指示加厚造山根深部延向与规模拆沉轮廓，磨子潭-晓天断裂属于伸展后造山带主缝合线残留。斜向汇聚使得大别区俯冲深度深于红安区，由此导致大别区(超)高压折返要比红安区更具规模性，这种差异折返还有助于理解大别造山带差异热窿伸展作用。大别造山机制经历过由早期俯冲型造山(Subduction)到晚期挤入型造山(Indentation)的转变过程。
The Dabieshan orogen, located between North China plate and Yangtze plate, has become thefocus of geological research due to unique exposure of large-scale HP/UHP rocks and itsrelationship with NNE trending Tanlu fault. Reconstruction of an original distribution of HP/UHPunits and their PTt paths helps in the understanding of orogenic dynamics process. After HP/UHPorogenic exhumation, Dabieshan orogen entered into the period of thermal rebuilding driven byintense extension. This study emphasizes post-collisional tectonic-thermal and magmatic processrather than HP/UHP units themselves through combined geochronology, structure analysis andgeochemistry studies. This study is essential to reconstruct post-date-orogenic evolution history,and also essential to restore the original HP/UHP distribution and exhumation models. Therefore,it can provide detailed constraints on Dabieshan orogenesis mechanism. Our major researchconclusions are as follows.
a) Based on regional geochronology, the Dabieshan orogen underwent thermal doming extensionduring 140～85Ma, which resulted in widespread re-melting of metamorphic basement, intensevolcanic activities in North Huaiyang and formation of fault-controlled depressions in Hefeibasin. This thermal doming event can be further divided into two consecutive evolving stages,i.e., the intensifying stage (140～105Ma) and the declining stage (105~85Ma). In 140～105Mastage, the thermal doming was mainly concentrated in the Dabie block, and to a less degree, inthe Hong'an block. The Dabie doming structure is configured with Macheng-Yuexi thermalaxis, Yuexi/Luotian thermal cores and their downslide flanks. The orientation of thermal axisruns dominantly parallel to the orogen Strike, and North Huaiyang and HP/UHP units constitutedownslide flanks. Yuexi core differs from Luotian core in both intensity and shaping time. Thedoming process of Dabieshan is characterized by thermal-center's migration along Macheng-Yuexi thermal axis. Consequently, it is speculated to be attributed to convective removal ofthickened orogen-root, which is a process characterized by intermittence, migration, large-scaleand differentiation. During 105～85Ma stage, the dome-shaped figure still structurally existed,but each tectonic units cooled remarkably slow and magmatic activities stagnated gradually.
b) Based on structure analysis of present outcrops, the Dabieshan orogen is dominated by thearchitecture of doming extension, which actually formed during Cretaceous period(140～85Ma).This doming architecture is structurally configured with doming cores, detachment faults anddownslide flanks. Moreover, the intensity of extension displays regional differentiation, strongin Dabie block but weak in Hong'an block. In Hong'an block, the doming structure comprisesFutianhe/Kafang cores and Hong'an group/north Huaiyang downslide systems, and Pingtianfan,Xiongdian-huwan, Fengdian-qiliping and Dawu-xishui faults constitute detachment faults. The(low)amphibolite facies chiefly developed within the core area, but the greenschist faciesconcentrated on the doming downslide systems. In Dabie block, its configuration of domingextension includes Luotian/Yuexi cores as well as north Huaiyang/(U)HP downslide units, andYingshan-xinzhou, Mozitan-xiaotian, Taihu-xishui faults obviously exhibit some attributes ofdetachment faults. The amphibolite facies mostly are distributed in the range of doming coreswith larger depth of exhumation, but low-amphibolite facies and greenschist facies come withthe doming downslide systems.
c) Apatite fission track (AFT) analysis shows that at 90Ma±the doming structure of Dabieshanwas replaced by another architecture, which is characterized by the thermal fault-depressionintersecting thermal short-axis uplift. This new architecture possibly continued into 90～32Maperiod, although thermal differentiation and small-scale domes occurred in its late stage. Forabove architecture, its driven mechanism is related to a regional differential push-up process,which possibly resulted from some changeable properties of convergence in the western Pacificmargin. This push-up process played an important role in the shaping of modern topography,too. Furthermore, AFt modeling history shows that the orogen of Dabieshan underwent otherthermal events. In detail, the 65～56Ma event found its intense expression near north/southboundary faults of orogen, and much intense in north Huaiyang and Hefei basin. Additionally,the 34～30Ma event almost affected the whole orogen of Dabieshan and its northern basins. The20～13Ma event, differently, thermally disturbed mainly within Dabie and Hong'an blocks, anddecreasing towards north Huaiyang and Hefei basin. These thermal events are presumed to be related to the India-Asia collision tectonics, the Pacific subduction tectonics and the open/closeprocess of South China Sea basin.
d) The tectonic/magmatic history of Dabieshan orogen (since Mesozoic era) generally can bedivided into 6 events, i.e., the convergence "island-arc" event(>240Ma), the slab "break-off"event(210Ma±), the compression "thickening" event(early~middle Jurassic), the "delaminationof orogen root"event(early Cretaceous), the far-field "extension" event(85~53Ma), and the"mantle plume" event(sine Oligocene epoch). The delamination of orogen root led to intensethermal extension in Dabieshan. Consequently, most of intermediate-basic (sub)volcanics areenriched in Ba、La、K_2O, and components of TiO_2, Nb、P_2O_5 display negative anomaly, andtheir isotopic sources have a strong affinity to EMI mantle and basement rocks. During late-Cretaceous and Paleocene, the K_2O content in volcanics decreased clearly, and their magmaticsources lay between BSE and EMI mantles. This volcanism was possibly under the control ofback-arc extension of western Pacific convergence. Since Oligocene, all volcanic rocks relatedto the mantle plume event represent component of ocean-island basalt, and they have a strongaffinity to PREMA mantle source.
e) During late-Jurassic-early Cretaceous period, volcanic rocks with EMI mantle directly resultedfrom combination of delamination material of orogen root and mantle source. In SoutheasternChina, the basic/intermediate volcanism, characterized by EMI-EMII transition source, wastectonically correlated with addition of subducted oceanic sediments, back-arc extension ofwestern Pacific, and uplifting of continental mantle. In the Lower Yangtze, however, volcanismdisplayed transition mantle source between "delaminaton of orogen root" mantle (Dabieshan)"and "back-arc extension" mantle (Southeastern China), and thus, we attempt to link evolutionof Dabieshan orogen with eastern continental margin by tectonic intersection and constraints.The orogen delamination was resulted from superimposed control of orogenic tectonics andextension of eastem continental margin. In late-Cretaceous～Paleocene, volcanic rocks fromDabieshan, Lower Yangtze to Southeast China, approached oceanic-island basalt, and had aclose affinity to BSE mantle. It can be concluded that the volanism(late-Cretaceous～Paleocene)of East China was gradually controlled by an identical mantle source and back-arc extensionalsetting. Since Oligocene, this volcanism is driven by the same mantle source and the sametectonic setting, and their volcanic rocks display the PREMA mantle source and component ofoceanic island basalt. Additionally, some peridotite inclusions imply existence of PREMAmantle in the〉700km depth. We relate these properties of volcanics to the mantle-plume event.
f) The Dabieshan orogen is speculated to represent the bivergent-belt architecture rather thanunilateral-wedge-extrusion model. Only detachment faulting, instead of one tectomc boundary,exists between "gay gneiss of North DaNe" and "UHP/HP units of South Dabie", which wastriggered by the thermal doming extension. The Macheng-Yuexi thermal axial represents the deeptrending orientation of thickened orogen root. Mozitan-xiaotian fault possibly serves as one partof remnant suture reconstructed by the thermal doming extension occurred during 140～85Ma.The subduction depth in Dabie block exceeds that in Hong'an block due to oblique convergence,therefore, HP/UHP exhumation scale in Dabie block may be larger than that in Hong'an block.This fact also helps to explain differential thermal extension existed between DaNe block andHong'an block. The Dabieshan orogen might underwent transition from mantle-subduction typeinto indentation type.
(1)热年代学分析表明：140～85Ma大别造山带进入热窿伸展时期，由此引发广泛基底熔融、火山剧烈喷溢与盆地断陷作甩，这次热窿事件包括强热伸展阶段(140～105Ma)和晚期衰退阶段(105～85Ma)。在强热伸展阶段，热窿作用集中在大别／红安地块，并以大别地块最为强烈。大别热窿鱼括麻城-岳西热轴、穹核组合以及外围下滑系统，热轴平行造山带延向展布，北淮阳与(超)高压单元构成下滑系统，岳西、罗田热窿核占据麻城-岳西热轴东、西两端，它们最终成型时代不一致。热窿伸展进程伴随着大别强热中心沿着热伸展轴迁移摆动，这说明造山根拆沉过程以间歇性、迁移性、规模性与区域差异性为特征。在伸展退阶段，大别山仍显现穹状轮廓，但伸展强度与岩浆作用显著减弱。
(2)构造解析表明：在现今剥露面内，大别山以伸热窿格局(140～85Ma)为主导，包括热窿核→剥离断裂带→下滑系统配置单元，热窿作用在商麻断裂两侧差异性显著。红安区热窿包括福田河／卡房窿核与红安群／北淮阳下滑系统，平天畈、熊店-浒湾、丰店-七里坪以及大悟-浠水等断裂构成滑脱带，(低)角闪岩相热伸展集中在窿核处，在下滑系统中发育绿片岩相伸展。大别区热窿由罗田／岳西窿核与北淮阳／南大别(超)高压下滑单元构成，其间(内)存在英山-新洲、磨子潭-晓天、太湖-浠水等滑脱带。大别热窿由中深到浅层次剥露过程对应着角闪岩相、低角闪岩相到绿片岩相退变质序列。
(3)低温年代学分析表明：90Ma±造山带热窿构造最终被热断陷交切短轴热隆格局所取代，这种构造格局可一直延续到K～E(90～32Ma)时期(后期出现热分异与穹窿组合)，其形成机制应该与西太平洋域汇聚特性引发区域差异推隆作用相关，这种推隆过程对于大别山现代地形建立有重要贡献。大别山AFT模拟热史还记录其它三次热构造事件：古新世(58～65Ma)热事件在造山带南北侧近边界断裂处影响显著，并在北淮阳与北缘盆地最为强烈；渐新世(30～34Ma)热事件广泛影响到整个造山带与北侧盆地；中新世(13～20Ma)热扰动集中在大别、红安两地块，而在北淮阳与合肥盆地相当微弱；推测这些热构造事件应该与西部碰撞域、东部汇聚域以及南海盆地扩张／关闭远场响应有关。
(4)地球化学分析表明，大别造山带构造／岩浆事件(中生代以来)包括六期，汇聚“岛弧”事件(〉240Ma)、板块“断离”事件(210Ma±)、挤压“加厚”事件(早～中侏罗世)、造山带“去根”事件(早白垩世)、远场“扩张”事件(85～53Ma)与“地幔羽”事件(渐新世以来)。大别山热窿伸展与造山带“去根”作用密切相关，岩浆显示TiO_2、Nb、P_2O_5亏损、Ba、La、K_2O富集特点，岩浆源区显著亲合于EMI端元和下地壳。进入晚白垩世～古新世，由于受西太平洋汇聚域弧后扩张作用制约，火山岩钾质含量减少，岩浆源区位于BSE与EMI之间。渐新世以来，地幔羽事件以岩浆显著亲合PREMA幔源和洋岛玄武岩为标志。
(5)对比邻区表明：①晚侏罗世～早白垩世，大别山源源(EMI)岩浆形成与造山根拆沉熔入地幔再循环有关，东南区幔源(EMI与EMII过渡)岩浆特性应该与洋壳俯冲沉积物加入、西太平洋汇聚域弧后扩张、以及大陆地幔上隆作用相联系，而下扬子岩浆兼有“拆沉”混合幔源(大别山)与弧后扩张幔源(东南区)过渡性质。大别造山带演化与东部大陆边缘显现构造制约关系，造山带“去根”作用属于造山晚后期构造与西太平洋域弧后扩张叠置产物。②晚白垩世～古新世，大别山与下扬子、东南区火山岩趋向洋岛玄武岩组成，同位素向着εNd增加、~(87)sr~(86)Sr减少方向演化，地幔源区与BSE端元大致亲合。这一时期，我国东部火山作用逐渐趋于统一幔源与统一扩张环境，而大别山晚后造山期演化渐趋于终结。③渐新世以来，统一构造环境与同一幔源区控制着我国东部火山作用，该时期火山岩显著亲合于PREMA幔源和洋岛玄武岩组成，橄榄岩包体指示深部存在PREMA地幔端元，这种特性应该与西太平洋域弧后扩张、地幔羽作用密切相关。
(6)构造剥离分析表明：大别造山带具有双侧造山特点，(超)高压单元与灰色片麻岩之间为热窿核与下滑系统配置关系，南北大别界限可能不存在。麻城-岳西热轴指示加厚造山根深部延向与规模拆沉轮廓，磨子潭-晓天断裂属于伸展后造山带主缝合线残留。斜向汇聚使得大别区俯冲深度深于红安区，由此导致大别区(超)高压折返要比红安区更具规模性，这种差异折返还有助于理解大别造山带差异热窿伸展作用。大别造山机制经历过由早期俯冲型造山(Subduction)到晚期挤入型造山(Indentation)的转变过程。
The Dabieshan orogen, located between North China plate and Yangtze plate, has become thefocus of geological research due to unique exposure of large-scale HP/UHP rocks and itsrelationship with NNE trending Tanlu fault. Reconstruction of an original distribution of HP/UHPunits and their PTt paths helps in the understanding of orogenic dynamics process. After HP/UHPorogenic exhumation, Dabieshan orogen entered into the period of thermal rebuilding driven byintense extension. This study emphasizes post-collisional tectonic-thermal and magmatic processrather than HP/UHP units themselves through combined geochronology, structure analysis andgeochemistry studies. This study is essential to reconstruct post-date-orogenic evolution history,and also essential to restore the original HP/UHP distribution and exhumation models. Therefore,it can provide detailed constraints on Dabieshan orogenesis mechanism. Our major researchconclusions are as follows.
a) Based on regional geochronology, the Dabieshan orogen underwent thermal doming extensionduring 140～85Ma, which resulted in widespread re-melting of metamorphic basement, intensevolcanic activities in North Huaiyang and formation of fault-controlled depressions in Hefeibasin. This thermal doming event can be further divided into two consecutive evolving stages,i.e., the intensifying stage (140～105Ma) and the declining stage (105~85Ma). In 140～105Mastage, the thermal doming was mainly concentrated in the Dabie block, and to a less degree, inthe Hong'an block. The Dabie doming structure is configured with Macheng-Yuexi thermalaxis, Yuexi/Luotian thermal cores and their downslide flanks. The orientation of thermal axisruns dominantly parallel to the orogen Strike, and North Huaiyang and HP/UHP units constitutedownslide flanks. Yuexi core differs from Luotian core in both intensity and shaping time. Thedoming process of Dabieshan is characterized by thermal-center's migration along Macheng-Yuexi thermal axis. Consequently, it is speculated to be attributed to convective removal ofthickened orogen-root, which is a process characterized by intermittence, migration, large-scaleand differentiation. During 105～85Ma stage, the dome-shaped figure still structurally existed,but each tectonic units cooled remarkably slow and magmatic activities stagnated gradually.
b) Based on structure analysis of present outcrops, the Dabieshan orogen is dominated by thearchitecture of doming extension, which actually formed during Cretaceous period(140～85Ma).This doming architecture is structurally configured with doming cores, detachment faults anddownslide flanks. Moreover, the intensity of extension displays regional differentiation, strongin Dabie block but weak in Hong'an block. In Hong'an block, the doming structure comprisesFutianhe/Kafang cores and Hong'an group/north Huaiyang downslide systems, and Pingtianfan,Xiongdian-huwan, Fengdian-qiliping and Dawu-xishui faults constitute detachment faults. The(low)amphibolite facies chiefly developed within the core area, but the greenschist faciesconcentrated on the doming downslide systems. In Dabie block, its configuration of domingextension includes Luotian/Yuexi cores as well as north Huaiyang/(U)HP downslide units, andYingshan-xinzhou, Mozitan-xiaotian, Taihu-xishui faults obviously exhibit some attributes ofdetachment faults. The amphibolite facies mostly are distributed in the range of doming coreswith larger depth of exhumation, but low-amphibolite facies and greenschist facies come withthe doming downslide systems.
c) Apatite fission track (AFT) analysis shows that at 90Ma±the doming structure of Dabieshanwas replaced by another architecture, which is characterized by the thermal fault-depressionintersecting thermal short-axis uplift. This new architecture possibly continued into 90～32Maperiod, although thermal differentiation and small-scale domes occurred in its late stage. Forabove architecture, its driven mechanism is related to a regional differential push-up process,which possibly resulted from some changeable properties of convergence in the western Pacificmargin. This push-up process played an important role in the shaping of modern topography,too. Furthermore, AFt modeling history shows that the orogen of Dabieshan underwent otherthermal events. In detail, the 65～56Ma event found its intense expression near north/southboundary faults of orogen, and much intense in north Huaiyang and Hefei basin. Additionally,the 34～30Ma event almost affected the whole orogen of Dabieshan and its northern basins. The20～13Ma event, differently, thermally disturbed mainly within Dabie and Hong'an blocks, anddecreasing towards north Huaiyang and Hefei basin. These thermal events are presumed to be related to the India-Asia collision tectonics, the Pacific subduction tectonics and the open/closeprocess of South China Sea basin.
d) The tectonic/magmatic history of Dabieshan orogen (since Mesozoic era) generally can bedivided into 6 events, i.e., the convergence "island-arc" event(>240Ma), the slab "break-off"event(210Ma±), the compression "thickening" event(early~middle Jurassic), the "delaminationof orogen root"event(early Cretaceous), the far-field "extension" event(85~53Ma), and the"mantle plume" event(sine Oligocene epoch). The delamination of orogen root led to intensethermal extension in Dabieshan. Consequently, most of intermediate-basic (sub)volcanics areenriched in Ba、La、K_2O, and components of TiO_2, Nb、P_2O_5 display negative anomaly, andtheir isotopic sources have a strong affinity to EMI mantle and basement rocks. During late-Cretaceous and Paleocene, the K_2O content in volcanics decreased clearly, and their magmaticsources lay between BSE and EMI mantles. This volcanism was possibly under the control ofback-arc extension of western Pacific convergence. Since Oligocene, all volcanic rocks relatedto the mantle plume event represent component of ocean-island basalt, and they have a strongaffinity to PREMA mantle source.
e) During late-Jurassic-early Cretaceous period, volcanic rocks with EMI mantle directly resultedfrom combination of delamination material of orogen root and mantle source. In SoutheasternChina, the basic/intermediate volcanism, characterized by EMI-EMII transition source, wastectonically correlated with addition of subducted oceanic sediments, back-arc extension ofwestern Pacific, and uplifting of continental mantle. In the Lower Yangtze, however, volcanismdisplayed transition mantle source between "delaminaton of orogen root" mantle (Dabieshan)"and "back-arc extension" mantle (Southeastern China), and thus, we attempt to link evolutionof Dabieshan orogen with eastern continental margin by tectonic intersection and constraints.The orogen delamination was resulted from superimposed control of orogenic tectonics andextension of eastem continental margin. In late-Cretaceous～Paleocene, volcanic rocks fromDabieshan, Lower Yangtze to Southeast China, approached oceanic-island basalt, and had aclose affinity to BSE mantle. It can be concluded that the volanism(late-Cretaceous～Paleocene)of East China was gradually controlled by an identical mantle source and back-arc extensionalsetting. Since Oligocene, this volcanism is driven by the same mantle source and the sametectonic setting, and their volcanic rocks display the PREMA mantle source and component ofoceanic island basalt. Additionally, some peridotite inclusions imply existence of PREMAmantle in the〉700km depth. We relate these properties of volcanics to the mantle-plume event.
f) The Dabieshan orogen is speculated to represent the bivergent-belt architecture rather thanunilateral-wedge-extrusion model. Only detachment faulting, instead of one tectomc boundary,exists between "gay gneiss of North DaNe" and "UHP/HP units of South Dabie", which wastriggered by the thermal doming extension. The Macheng-Yuexi thermal axial represents the deeptrending orientation of thickened orogen root. Mozitan-xiaotian fault possibly serves as one partof remnant suture reconstructed by the thermal doming extension occurred during 140～85Ma.The subduction depth in Dabie block exceeds that in Hong'an block due to oblique convergence,therefore, HP/UHP exhumation scale in Dabie block may be larger than that in Hong'an block.This fact also helps to explain differential thermal extension existed between DaNe block andHong'an block. The Dabieshan orogen might underwent transition from mantle-subduction typeinto indentation type.
引文
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