准噶尔盆地白垩纪——新近纪地层颜色韵律与古环境和古气候演化
|
摘要
准噶尔盆地南缘白垩纪—新近纪发育大型陆相浅水湖盆,干湿与冷暖气候频繁交替,形成了多套色彩斑斓的"五彩"地层,如灰色、灰绿色、灰白色、酱红色、红褐色、砖红色、紫红色、土黄色等。研究表明:地层颜色具有很好的沉积环境指示意义,如颜色指标L*(黑白),a*(红绿)以及b*(蓝黄)可以明显区分不同的水下与水上沉积环境(如水上河流—三角洲相、泛滥平原、山麓—冲积扇相等,水下半深湖相、滨浅湖相等);地层颜色演化序列可以很好地指示白垩纪—新近纪古气候的演化过程。红色沉积物既可以形成于干旱炎热的陆上氧化环境,也可以形成于相对还原的水下环境:"陆上红"如东沟组砖红色砂泥岩、紫泥泉子组紫红色泥岩、沙湾组褐红色—土红色泥岩等,40>L*> 52,8>a*> 18,12>b*> 22;"水下红"以呼图壁河组酱红色块状泥岩为特征,35>L*> 45,2. 5>a*> 4. 5,5>b*> 9。早白垩世准噶尔盆地相对温暖湿润,湖泊广泛分布,颜色指标L*(黑白)最低值接近15,a*值介于-5～5之间,指示深灰色—灰黑色泥岩形成于还原环境。晚白垩世地层颜色指标中a*达到了最高峰(15～25),表明准噶尔盆地气候开始出现干旱炎热趋势;古近纪始新世—渐新世,a*与b*值同步变化,出现了明显的负漂趋势(7～15),表明气候逐渐变冷;新近纪a*值出现新低(5～9),而L*值也接近70,表明气候持续变冷。综上所述,白垩纪末期以来,准噶尔盆地受全球气候变冷和青藏高原隆升共同影响,干旱化程度不断加强,地层颜色比较完整地保留和记录了古环境与古气候的发展演化过程。因此,系统的颜色测量和分析可以为恢复与重建中新生代沉积环境与古气候演化提供重要依据,对于探究新生代以来全球气候变化规律也具有重要意义。
The southern margin of the Junggar Basin in the Cretaceous-Neogene developed large continental shallow-water lacustrine basins with frequent alternation of dry and wet,cold and warm climate,forming a series of "multicolor"strata,such as gray,grey-green,grey-white,maroon red,red-brown,brick-red,purple-red,and earthy yellow. The study shows that the color of the strata has a good indicator of sedimentary environment. For example,the color index L* (black and white),a* (red and green)and b* (blue and yellow) can clearly distinguish the different subaquatic (semi-deep lacustrine facies,shore-shallow lacustrine facies) or subaerial (river-delta facies,floodplain facies,alluvial fan facies)sedimentary environments. Stratigraphic color evolution sequence can indicate the evolution of CretaceousNeogene palaeoclimate. The red sediments can be formed in both the dry and hot land oxidation environment and the relatively reduced underwater environment: "subaerial red",such as brick red sandy mudstone of the Donggou Formation,purple red mudstone of the Ziniquanzi Formation,and maroon to earth red mudstone of the Shawan Formation,40>L*> 52,8>a*> 18,12>b*> 22; "subaquatic red"is characterized by the thick red blocky mudstone of the Hutubihe Formation,35>L*> 45,2. 5>a*> 4. 5,5 >b*> 9. In the Early Cretaceous,the Junggar Basin was relatively warm and humid with wide distribution of lakes. The minimum value of the color index L* (black and white) was close to 15,and the value of a*was between-5 and 5,indicating that dark gray to gray dark mudstone was formed in a relatively reducting environment. In the Late Cretaceous,the color index a*reached the highest peak (15-25),indicating that the climate of the Junggar Basin began to show a trend of drought and heat. During the Eocene to Oligocene,the values of a*and b*changed synchronously,and there was an obvious trend of negative drift (7-15),and the climate gradually cooled. In the Neogene,the color index a*was relatively low (5-9),however,the L*value was close to 70,indicating that the climate continued to be cool. The research shows that since the end of Cretaceous,the drought-stricken Junggar Basin has been increasingly affected by the global climate cooling and the uplift of Qinghai-Tibet Plateau. The stratigraphic color recorded evolution of paleoenvironment and paleoclimate. Systematic color measurement and analysis can provide an important basis for reconstruction of Mesozoic-Cenozoic sedimentary environment and paleoclimate evolution. It also has a great significance for exploration of global climate change since the Cenozoic.
The southern margin of the Junggar Basin in the Cretaceous-Neogene developed large continental shallow-water lacustrine basins with frequent alternation of dry and wet,cold and warm climate,forming a series of "multicolor"strata,such as gray,grey-green,grey-white,maroon red,red-brown,brick-red,purple-red,and earthy yellow. The study shows that the color of the strata has a good indicator of sedimentary environment. For example,the color index L* (black and white),a* (red and green)and b* (blue and yellow) can clearly distinguish the different subaquatic (semi-deep lacustrine facies,shore-shallow lacustrine facies) or subaerial (river-delta facies,floodplain facies,alluvial fan facies)sedimentary environments. Stratigraphic color evolution sequence can indicate the evolution of CretaceousNeogene palaeoclimate. The red sediments can be formed in both the dry and hot land oxidation environment and the relatively reduced underwater environment: "subaerial red",such as brick red sandy mudstone of the Donggou Formation,purple red mudstone of the Ziniquanzi Formation,and maroon to earth red mudstone of the Shawan Formation,40>L*> 52,8>a*> 18,12>b*> 22; "subaquatic red"is characterized by the thick red blocky mudstone of the Hutubihe Formation,35>L*> 45,2. 5>a*> 4. 5,5 >b*> 9. In the Early Cretaceous,the Junggar Basin was relatively warm and humid with wide distribution of lakes. The minimum value of the color index L* (black and white) was close to 15,and the value of a*was between-5 and 5,indicating that dark gray to gray dark mudstone was formed in a relatively reducting environment. In the Late Cretaceous,the color index a*reached the highest peak (15-25),indicating that the climate of the Junggar Basin began to show a trend of drought and heat. During the Eocene to Oligocene,the values of a*and b*changed synchronously,and there was an obvious trend of negative drift (7-15),and the climate gradually cooled. In the Neogene,the color index a*was relatively low (5-9),however,the L*value was close to 70,indicating that the climate continued to be cool. The research shows that since the end of Cretaceous,the drought-stricken Junggar Basin has been increasingly affected by the global climate cooling and the uplift of Qinghai-Tibet Plateau. The stratigraphic color recorded evolution of paleoenvironment and paleoclimate. Systematic color measurement and analysis can provide an important basis for reconstruction of Mesozoic-Cenozoic sedimentary environment and paleoclimate evolution. It also has a great significance for exploration of global climate change since the Cenozoic.
引文
曹琦,郑龙君,王金玲.2014.沉积岩中颜色与成因的关系.黑龙江科技信息,28:105-106.[Cao Q,Zheng L J,Wang J L.2014.The relationship between sedimentary rock color and origin.Heilongjiang Science and Technology Information,28:105-106]
陈杰,杨太保,曾彪,何毅,冀琴.2018.中国帕米尔地区黄土上部色度变化特征及古气候意义.沉积学报,36(2):333-342.[Chen J,Yang T B,Zeng B,He Y,Ji Q.2018.Chroma characteristics and its paleoclimatic significance in Pamir Loess Section,China.Acta Sedimentologica Sinica,36(2):333-342]
陈一萌,陈兴盛,宫辉力,魏明建,李小娟.2006.土壤颜色:一个可靠的气候变化代用指标.干旱区地理,29(3):309-319.[Chen YM,Chen X S,Gong H L,Wei M J,Li X J.2006.Soil color:A new sensitive indicator for climatic change.Arid Land Geography,29(3):309-319]
邓松涛,吴朝东,顾潇,郭召杰.2008.晚新生代以来天山北缘沉积记录及其稳定同位素变化的环境意义.岩石学报,24(4):689-698.[Deng S T,Wu C D,Gu X,Guo Z J.2008.Sedimentary records and paleoenvirnmental significance of stable isotopic evidences from the Late Cenozoic,northern Tianshan.Acta Petrologica Sinica,24(4):689-698]
邓远,陈世悦,杨景林,王越.2015.准噶尔盆地北部晚白垩世-古近纪沉积特征.岩性油气藏,27(5):53-59.[Deng Y,Chen S Y,Yang J L,Wang Y.2015.Sedimentary characteristics of Late Cretaceous and Paleogene in northern Junggar Basin.Lithologic Reservoirs,27(5):53-59]
丁敏,庞奖励,黄春长,彭淑贞,杨炯,陈栋栋.2010.全新世黄土-古土壤序列色度特征及气候意义:以关中平原西部梁村剖面为例.陕西师范大学学报,38(5):92-97.[Ding M,Pang J L,Huang C C,Peng S Z,Yang J,Chen D D.2010.Chroma characteristics and its climatic significance in Holocene loess-paleosol sequence:A case study of the Holocene Liangcun profile in the western Guanzhong Basin.Journal of Shaanxi Normal University,38(5):92-97]
方世虎,郭召杰,张志诚,徐怀民,刘楼军.2004.准噶尔盆地中生代演化的地层学和沉积学证据.高校地质学报,10(4):554-561.[Fang S H,Guo Z J,Zhang Z C,Xu H M,Liu L J.2004.Mesozoic tectonic evolution of southern Junggar Basin,northwestern China:Constraints from stratigraphic and sedimentologic evidences.Geological Journal of China Universities,10(4):554-561]
方世虎,郭召杰,吴朝东,张志诚,王美娜,袁庆东.2006a.准噶尔盆地南缘侏罗系碎屑成分特征及其对构造属性、盆山格局的指示意义.地质学报,80(2):196-209.[Fang S H,Guo Z J,Wu CD,Zhang Z C,Wang M N,Yuan Q D.2006a.Jurassic clastic composition in the southern Junggar Basin,Northwest China:Implications for basin-range pattern and tectonic attributes.Acta Geologica Sinica,80(2):196-209]
方世虎,郭召杰,贾承造,张志诚,王绪龙,王美娜.2006b.准噶尔盆地南缘中-新生界沉积物重矿物分析与盆山格局演化.地质科学,41(4):648-662.[Fang S H,Guo Z J,Jia C Z,Zhang Z C,Wang X L,Wang M N.2006b.Meso-Cenozoic heavy minerals’assemblages in the southern Junggar Basin and its implications for basin-orogen pattern.Chinese Journal of Geology,41(4):648-662]
方小敏,潘保田,管东红,李吉军,小野有五,福泽仁之,大井圭一.1999.兰州约60 ka以来夏季风干年尺度不稳定性研究.科学通报,44(4):436-439.[Fang X M,Pan B T,Guan D H,Li J J,Yogo One,Fortune Hitoshi,Keiichi Ooi.1999.Study on the millennial scale instability of summer monsoon in Lanzhou since 60 ka.Chinese Science Bulletin,44(4):436-439]
付旭东,周广胜,张新时.2016.浑善达克沙地沙丘剖面颜色变化的古气候意义.沉积学报,34(1):70-78.[Fu X D,Zhou G S,Zhang X S.2016.Color variations of paleosol-sand profiles across Otindag Sandy Land and its paleoclimatic implications.Acta Sedimentologica Sinica,34(1):70-78]
高鹏坤,庞奖励,黄春长,周亚利,卞鸿雁,王蕾彬,王学佳.2015.陕南丹凤茶房村黄土-古土壤剖面色度参数特征.沉积学报,33(3):537-542.[Gao P K,Pang J L,Huang C C,Zhou Y L,Bian H Y,Wang L B,Wang X J.2015.Chroma characteristics and its significance of Chafangcun loess-paleosol profile in Shaanxi,China.Acta Sedimentologica Sinica,33(3):537-542]
高志勇,周川闽,冯佳睿,吴昊,李雯.2016.中新生代天山隆升及其南北盆地分异与沉积环境演化.沉积学报,34(3):415-435.[Gao Z Y,Zhou C M,Fen J R,Wu H,Li W.2016.Relationship between the Tianshan mountains uplift and depositional environment evolution of the basins in Mesozoic-Cenozoic.Acta Sedimentologica Sinica,34(3):415-435]
谷云飞,马明福,苏世龙,徐怀民,胡斌,姚卫江.2003.准噶尔盆地白垩系岩相古地理.石油实验地质,25(4):338-347.[Gu Y F,Ma M F,Su S L,Xu H M,Hu B,Yao W J.2003.Lithofacies paleogeography of the Cretaceous in the Junggar Basin.Petroleum Geology&Experiment,25(4):338-347]
郭召杰,张志诚,吴朝东,方世虎,张锐.2006.中、新生代天山隆升过程及其与准噶尔、阿尔泰山比较研究.地质学报,80(1):1-15.[Guo Z J,Zhang Z C,Wu C D,Fang S H,Zhang R.2006.The Mesozoic and Cenozoic exhumation history of Tianshan and comparative studies to the Junggar and Altai Mountains.Acta Geologica Sinica,80(1):1-15]
季军良,朱敏,王旭,罗攀,董欣欣.2010.准噶尔盆地南缘新生代地层时代研究.地层学杂志,34(1):43-50.[Ji J L,Zhu M,Wang X,Luo P,Dong X X.2010.Ages of the Cenozoic strata on the southern margin of Junggar Basin,northwstern China.Journal of Stratigraphy,34(1):43-50]
李国荣.2012.浅析沉积岩颜色与沉积相的关系.内江科技,(5):49-50.[Li G R.2012.The relationship between sedimentary rock color and sedimentary facies.Neijiang Science and Technology,(5):49-50]
李骞,田孝茹,胡瀚文,郭召杰.2016.天山北缘安集海河组湖相灰岩氧碳同位素变化的古环境意义.地球科学与环境学报,38(3):339-408.[Li Q,Tian X R,Hu H W,Guo Z J.2016.Paleoenvironmental significance of oxygen and carbon isotopic records in lacustrine limestone from Anjihaihe Formation,northern Tianshan.Journal of Earth Science and Environment,38(3):339-408]
李双建,张杰,王清晨.2006.沉积物颜色和粘土矿物对库车坳陷第三纪气候变化的指示.沉积学报,24(4):521-530.[Li S J,Zhang J,Wang Q C.2006.Implications of the color of sediments and clay minerals for Tertiary climatic changes of Kuqa Depression.Acta Sedimentologica Sinica,24(4):521-530]
李忠,彭守涛.2013.天山南北麓中-新生界碎屑锆石U-Pb年代学记录、物源体系分析与陆内盆山演化.岩石学报,29(3):739-755.[Li Z,Peng S T.2013.U-Pb geochronological records and provenance system analysis of the Mesozoic-Cenozoic sandstone detrital zircons in the northern and southern piedmonts of Tianshan,Northwest China:Responses to intracontinental basinrange evolution.Acta Petrologica Sinica,29(3):739-755]
马英俊,郑国东,刘芊.2006.吐鲁番盆地侏罗系沉积岩的颜色与铁的赋存状态关系研究.矿物学报,26(2):137-144.[Ma Y J,Zheng G D,L Q.2006.Relationship between the forms of occurrence of iron species and the colors of Jurassic sedimentary rocks in the Turpan Basin,Northwestern China.Acta Mineralogica Sinica,26(2):137-144]
宋春晖,白晋锋,赵彦德,金洪波,孟庆泉.2005.临夏盆地13~4.4 Ma湖相沉积物颜色记录的气候变化探讨.沉积学报,23(3):507-513.[Song C H,Bai J F,Zhao Y D,Jin H B,Meng QQ.2005.The color of lacustrine sediments recorded climatic changes from 13 to 4.5 Myr in Linxia Basin.Acta Sedimentologica Sinica,23(3):507-513]
徐丽,苗运法,方小敏,宋春晖,夏维民,闫晓丽,韩文霞,张启波,陈传飞,戴霜.2009.青藏高原东北部西宁盆地中始新世-渐新世沉积物颜色与气候变化.兰州大学学报,45(1):12-20.[Xu L,Miao Y F,Fang X M,Song C H,Xia W M,Yan X L,Han W X,Zhang Q B,Chen C F,Dai X.2009.Middle Eocene-Oligocene climatic changes recorded by sedimentary colors in the Xinjiang Basin,in northestern Tibetan Plateau,NW China.Journal of Lanzhou University,45(1):12-20]
王成善,胡修棉.2005.白垩纪世界与大洋红层.地学前缘,12(2):11-21.[Wang C S,Hu X M.2005.Cretaceous world and oceanic red beds.Earth Science Frontiers,12(2):11-21]
王成善,曹珂,黄永建.2009.沉积记录与白垩纪地球表层系统变化.地学前缘,16(5):1-14.[Wang C S,Cao K,Huang Y J.2009.Sedimentary record and Cretaceous earth surface System changes.Earth Science Frontiers,16(5):1-14]
王明振,吴朝东,房亚男,王陆新,李林林,陈榕,王军.2013.准噶尔盆地南缘坡缕石矿物学特征及古气候指示意义.岩石矿物学杂志,32(6):833-841.[Wang M Z,Wu C D,Fang Y N,Wang LX,Li L L,Chen R,Wang J.2013.Mineralogical characteristics of palygorskite in the southern margin of Junggar Basin and their implications for paleoclimate.Acta Petrologica et Mineralogica,32(6):833-841]
新疆维吾尔自治区地质矿产局.1999.新疆维吾尔自治区岩石地层.湖北武汉:中国地质大学出版社.[Bureau of Geology and Mineral Resources of Xinjiang Uygur Autonomous Region.1999.Lithostratigraphy of Xinjiang Uygur Autonomous Region.Wuhan of Hubei:China University of Geosciences Press]
许书堂,焦存礼,王敬缺.1998.伊犁盆地沉积岩颜色指数特征、盆地演化与有利勘探层系.勘探家,3(3):60-63.[Xu S T,Jiao CL,Wang J Q.1998.Sedimentary rock color index feature,basin evolution and favorable exploration strata in the Yili Basin.Petroleum Explorationist,3(3):60-63]
杨胜利,方小敏,李吉均,安芷生,陈诗越,福泽仁之.2001.表土颜色和气候定性至半定量关系研究.中国科学(D辑),31(增刊):175-181.[Yang S L,Fang X M,Li J J,An Z S,Chen S Y,Fortune Hitoshi.2001.Transformation functions of soil color and climate.Science in China(Series D),31(Suppl.):175-181]
雍天寿.1987.准噶尔盆地晚古生代-新生代岩相古地理.新疆石油地质,8(2):24-34.[Yong T S.1987.Junggar Basin Late Paleozoic-Cretaceous lithofacies and palaeogeography.Xinjiang Petroleum Geology,8(2):24-34]
An Z S,Kutzbach J E,Prell W L,Porter S C.2001.Evolution of Asian monsoons and phased up lift of the Himalaya-Tibetan plateau since Late Miocene times.Nature,411:62-66.
Avouac J P,Tapponnier P,Bai M,You H,Wang G.1993.Active thrusting and folding along the northern Tien Shan and Late Cenozoic rotation of the Tarim relative to Dzungaria and Kazakhstan.Journal of Geophysical Research:Solid Earth,98:6755-6804.
Bian W H,Hornung J,Liu Z H,Wang P J,Hinderer M.2010.Sedimentary and palaeoenvironmental evolution of the Junggar Basin,Xinjiang,Northwest China.Palaeogeography,Palaeoclimatology,Palaeoecology,90:175-186.
Charreau J,Chen Y,Gilder S,Dominguez S,Avouac J P,Sen S,Sun D J,Li Y A,Wang W M.2004.Magnetostratigraphy and rock magnetism of the Neogene Kuitun He section(northwest China):Implications for Late Cenozoic uplift of the Tianshan mountains.Earth and Planetary Science Letters,230:177-192.
Charreau J,Kent-Corson M L,Barrier R,Augier R,Ritts B D,Chen Y,France-Lannord C,Guilmette C.2012.A high-resolution stable isotopic record from the Junggar Basin(NW China):Implications for the paleotopographic evolution of the Tianshan Mountains.Earth and Planetary Science Letters,341-344:158-169.
Dewey J F,Shackelton R M,Chang C,Sun Y.1988.The tectonic evolution of the Tibetan Plateau.Phil.Trans.R.Soc.Lond.,A327:379-413.
Ding Z L,Yang S L,Hou S S,Chen Z,Liu T S.2001.Magnetostratigraphy and sedimentology of the Jingchuan red clay section and correlation of Tertiary eolian red clay sediments of the Chinese Loess Plateau.Journal of Geophysical Research:Solod Earth,106(B4):6399-6407.
Fang Y N,Wu C D,Wang Y Z,Wang L X,Guo Z J,Hu H W.2016.Stratigraphic and sedimentary characteristics of the Upper Jurassic-Lower Cretaceous strata in the Junggar Basin,Central Asia:Tectonic and climate implications.Journal of Asian Earth Sciences,129:294-308.
Frakes L A.1979.Climates throughout geologic time.Elsevier Scientific Pub.Co.10.1016/0025-3227(80)90114-0.
Guedes A,Ribeiro H,Valentim B,Noronha F.2009.Quantitative colour analysis of beach and dune sediments for forensic applications:APortuguese example.Forensic Science International,190:42-51.
Guo Z T,Ruddiman W F,Hao Q Z,Wu H B,Qiao Y S,Zhu R X,Peng SZ,Wei J J,Yuan B Y,Liu T S.2002.Onset of Asian desertification by 22 Myr ago inferred from loess deposits in China.Nature,416:159-163.
Haq B,Hardenbol J,Vail P.1988.Mesozoic and Cenozoic chronostratigraphy and cycles of sea-level change.SEPM Special Publication,42:71-108.
Ji J L,Pan L,Paul W,Jiang H C,Gao L,Ding Z L.2008.Episodic uplift of the Tianshan Mountains since the Late Oligocene constrained by magnetostratigraphy of the Jingou River section,in the southern margin of the Junggar Basin,China.Journal of Geophysical Research,113:B05102,doi:10.1029/2007JB005064.
Kent-Corson M L,Ritts B D,Zhuang G Z,Bovet P M,Graham S A,Chamberlain C P.2009.Stable isotopic constraints on the tectonic,topographic,and climatic evolution of the northern margin of the Tibetan Plateau.Earth and Planetary Science Letters,282(1-4):158-166.
Li J,Hu X M,Zhao K D,Cai Y F,Sun T.2016.Paleoceanographic evolution and chronostratigraphy of the Aptian Oceanic Anoxic Event 1a(OAE1a)to oceanic red bed 1(ORB1)in the Gorgo a Cerbara section(central Italy).Cretaceous Research,66:115-128.
Miller K G,Kominz M A,Browning J V,Wright J D,Mountain G S,Katz M E,Sugarman P J,Cramer B S,Christie-Blick N,Pekar S E.2005.The Phanerozoic record of global sea-level Change.Science,310:1293.
Myrow P M.1990.A new graph for understanding colors of mudrocks and shales.Journal of Geological Education,38:16-20.
Robertson A R.1977.The CIE 1976 color-difference formulae.Color research and Application,2(1):7-11.
Ruiz J F,Pereira J.2014.The colours of rock art:Analysis of colour recording and communication systems in rock art research.Journal of Archaeological Science,50:338-349.
Sun J M,Zhu R X,Bowler J.2004.Timing of the Tianshan Mountains uplift constrained by magnetostratigraphic analysis of molasse deposits.Earth and Planetary Science Letters,219(3-4):239-253.
Sun Y B,He L,Liang L J,An Z S.2011.Changing color of Chinese loess:Geochemical onstrint and paleoclimatic significance.Journal of Asian and Earth Sciences,40(6):1131-1138.
Tang Z H,Huang B C,Dong X X,Ji J L,Ding Z L.2012.Episodic uplift of the Tianshan Mountains since the Late Oligocene constrained by magnetostratigraphy of the Jingou River section,in the southern margin of the Junggar Basin,China.Journal of Geophysical Research,113,B05102.
Yang S L,Ding Z L.2003.Color reflectance of Chinese loess and its implications for climate gradient changes during the last two glacial-interglacial cycles.Geophysical Research Letters,30(20):2058.
Yu S,Chen W,Evans N J,Mcinnes B I A,Yin J Y,Sun J B,Li J,Zhang B.2014.Cenozoic uplift,exhumation and deformation in the north Kuqa Depression,China as constrained by(U-Th)/He thermochronometry.Tectonophysics,630:166-182.
Zheng G D,Fu B H,Duan Y,Wang Q,Matsuo M,Takano B.2004.Iron speciation related to color of Jurassic sedimentary rocks in Turpan Basin,northwest China.Journal of Radioanalytical and Nuclear Chemistry,261(2):421-427.
陈杰,杨太保,曾彪,何毅,冀琴.2018.中国帕米尔地区黄土上部色度变化特征及古气候意义.沉积学报,36(2):333-342.[Chen J,Yang T B,Zeng B,He Y,Ji Q.2018.Chroma characteristics and its paleoclimatic significance in Pamir Loess Section,China.Acta Sedimentologica Sinica,36(2):333-342]
陈一萌,陈兴盛,宫辉力,魏明建,李小娟.2006.土壤颜色:一个可靠的气候变化代用指标.干旱区地理,29(3):309-319.[Chen YM,Chen X S,Gong H L,Wei M J,Li X J.2006.Soil color:A new sensitive indicator for climatic change.Arid Land Geography,29(3):309-319]
邓松涛,吴朝东,顾潇,郭召杰.2008.晚新生代以来天山北缘沉积记录及其稳定同位素变化的环境意义.岩石学报,24(4):689-698.[Deng S T,Wu C D,Gu X,Guo Z J.2008.Sedimentary records and paleoenvirnmental significance of stable isotopic evidences from the Late Cenozoic,northern Tianshan.Acta Petrologica Sinica,24(4):689-698]
邓远,陈世悦,杨景林,王越.2015.准噶尔盆地北部晚白垩世-古近纪沉积特征.岩性油气藏,27(5):53-59.[Deng Y,Chen S Y,Yang J L,Wang Y.2015.Sedimentary characteristics of Late Cretaceous and Paleogene in northern Junggar Basin.Lithologic Reservoirs,27(5):53-59]
丁敏,庞奖励,黄春长,彭淑贞,杨炯,陈栋栋.2010.全新世黄土-古土壤序列色度特征及气候意义:以关中平原西部梁村剖面为例.陕西师范大学学报,38(5):92-97.[Ding M,Pang J L,Huang C C,Peng S Z,Yang J,Chen D D.2010.Chroma characteristics and its climatic significance in Holocene loess-paleosol sequence:A case study of the Holocene Liangcun profile in the western Guanzhong Basin.Journal of Shaanxi Normal University,38(5):92-97]
方世虎,郭召杰,张志诚,徐怀民,刘楼军.2004.准噶尔盆地中生代演化的地层学和沉积学证据.高校地质学报,10(4):554-561.[Fang S H,Guo Z J,Zhang Z C,Xu H M,Liu L J.2004.Mesozoic tectonic evolution of southern Junggar Basin,northwestern China:Constraints from stratigraphic and sedimentologic evidences.Geological Journal of China Universities,10(4):554-561]
方世虎,郭召杰,吴朝东,张志诚,王美娜,袁庆东.2006a.准噶尔盆地南缘侏罗系碎屑成分特征及其对构造属性、盆山格局的指示意义.地质学报,80(2):196-209.[Fang S H,Guo Z J,Wu CD,Zhang Z C,Wang M N,Yuan Q D.2006a.Jurassic clastic composition in the southern Junggar Basin,Northwest China:Implications for basin-range pattern and tectonic attributes.Acta Geologica Sinica,80(2):196-209]
方世虎,郭召杰,贾承造,张志诚,王绪龙,王美娜.2006b.准噶尔盆地南缘中-新生界沉积物重矿物分析与盆山格局演化.地质科学,41(4):648-662.[Fang S H,Guo Z J,Jia C Z,Zhang Z C,Wang X L,Wang M N.2006b.Meso-Cenozoic heavy minerals’assemblages in the southern Junggar Basin and its implications for basin-orogen pattern.Chinese Journal of Geology,41(4):648-662]
方小敏,潘保田,管东红,李吉军,小野有五,福泽仁之,大井圭一.1999.兰州约60 ka以来夏季风干年尺度不稳定性研究.科学通报,44(4):436-439.[Fang X M,Pan B T,Guan D H,Li J J,Yogo One,Fortune Hitoshi,Keiichi Ooi.1999.Study on the millennial scale instability of summer monsoon in Lanzhou since 60 ka.Chinese Science Bulletin,44(4):436-439]
付旭东,周广胜,张新时.2016.浑善达克沙地沙丘剖面颜色变化的古气候意义.沉积学报,34(1):70-78.[Fu X D,Zhou G S,Zhang X S.2016.Color variations of paleosol-sand profiles across Otindag Sandy Land and its paleoclimatic implications.Acta Sedimentologica Sinica,34(1):70-78]
高鹏坤,庞奖励,黄春长,周亚利,卞鸿雁,王蕾彬,王学佳.2015.陕南丹凤茶房村黄土-古土壤剖面色度参数特征.沉积学报,33(3):537-542.[Gao P K,Pang J L,Huang C C,Zhou Y L,Bian H Y,Wang L B,Wang X J.2015.Chroma characteristics and its significance of Chafangcun loess-paleosol profile in Shaanxi,China.Acta Sedimentologica Sinica,33(3):537-542]
高志勇,周川闽,冯佳睿,吴昊,李雯.2016.中新生代天山隆升及其南北盆地分异与沉积环境演化.沉积学报,34(3):415-435.[Gao Z Y,Zhou C M,Fen J R,Wu H,Li W.2016.Relationship between the Tianshan mountains uplift and depositional environment evolution of the basins in Mesozoic-Cenozoic.Acta Sedimentologica Sinica,34(3):415-435]
谷云飞,马明福,苏世龙,徐怀民,胡斌,姚卫江.2003.准噶尔盆地白垩系岩相古地理.石油实验地质,25(4):338-347.[Gu Y F,Ma M F,Su S L,Xu H M,Hu B,Yao W J.2003.Lithofacies paleogeography of the Cretaceous in the Junggar Basin.Petroleum Geology&Experiment,25(4):338-347]
郭召杰,张志诚,吴朝东,方世虎,张锐.2006.中、新生代天山隆升过程及其与准噶尔、阿尔泰山比较研究.地质学报,80(1):1-15.[Guo Z J,Zhang Z C,Wu C D,Fang S H,Zhang R.2006.The Mesozoic and Cenozoic exhumation history of Tianshan and comparative studies to the Junggar and Altai Mountains.Acta Geologica Sinica,80(1):1-15]
季军良,朱敏,王旭,罗攀,董欣欣.2010.准噶尔盆地南缘新生代地层时代研究.地层学杂志,34(1):43-50.[Ji J L,Zhu M,Wang X,Luo P,Dong X X.2010.Ages of the Cenozoic strata on the southern margin of Junggar Basin,northwstern China.Journal of Stratigraphy,34(1):43-50]
李国荣.2012.浅析沉积岩颜色与沉积相的关系.内江科技,(5):49-50.[Li G R.2012.The relationship between sedimentary rock color and sedimentary facies.Neijiang Science and Technology,(5):49-50]
李骞,田孝茹,胡瀚文,郭召杰.2016.天山北缘安集海河组湖相灰岩氧碳同位素变化的古环境意义.地球科学与环境学报,38(3):339-408.[Li Q,Tian X R,Hu H W,Guo Z J.2016.Paleoenvironmental significance of oxygen and carbon isotopic records in lacustrine limestone from Anjihaihe Formation,northern Tianshan.Journal of Earth Science and Environment,38(3):339-408]
李双建,张杰,王清晨.2006.沉积物颜色和粘土矿物对库车坳陷第三纪气候变化的指示.沉积学报,24(4):521-530.[Li S J,Zhang J,Wang Q C.2006.Implications of the color of sediments and clay minerals for Tertiary climatic changes of Kuqa Depression.Acta Sedimentologica Sinica,24(4):521-530]
李忠,彭守涛.2013.天山南北麓中-新生界碎屑锆石U-Pb年代学记录、物源体系分析与陆内盆山演化.岩石学报,29(3):739-755.[Li Z,Peng S T.2013.U-Pb geochronological records and provenance system analysis of the Mesozoic-Cenozoic sandstone detrital zircons in the northern and southern piedmonts of Tianshan,Northwest China:Responses to intracontinental basinrange evolution.Acta Petrologica Sinica,29(3):739-755]
马英俊,郑国东,刘芊.2006.吐鲁番盆地侏罗系沉积岩的颜色与铁的赋存状态关系研究.矿物学报,26(2):137-144.[Ma Y J,Zheng G D,L Q.2006.Relationship between the forms of occurrence of iron species and the colors of Jurassic sedimentary rocks in the Turpan Basin,Northwestern China.Acta Mineralogica Sinica,26(2):137-144]
宋春晖,白晋锋,赵彦德,金洪波,孟庆泉.2005.临夏盆地13~4.4 Ma湖相沉积物颜色记录的气候变化探讨.沉积学报,23(3):507-513.[Song C H,Bai J F,Zhao Y D,Jin H B,Meng QQ.2005.The color of lacustrine sediments recorded climatic changes from 13 to 4.5 Myr in Linxia Basin.Acta Sedimentologica Sinica,23(3):507-513]
徐丽,苗运法,方小敏,宋春晖,夏维民,闫晓丽,韩文霞,张启波,陈传飞,戴霜.2009.青藏高原东北部西宁盆地中始新世-渐新世沉积物颜色与气候变化.兰州大学学报,45(1):12-20.[Xu L,Miao Y F,Fang X M,Song C H,Xia W M,Yan X L,Han W X,Zhang Q B,Chen C F,Dai X.2009.Middle Eocene-Oligocene climatic changes recorded by sedimentary colors in the Xinjiang Basin,in northestern Tibetan Plateau,NW China.Journal of Lanzhou University,45(1):12-20]
王成善,胡修棉.2005.白垩纪世界与大洋红层.地学前缘,12(2):11-21.[Wang C S,Hu X M.2005.Cretaceous world and oceanic red beds.Earth Science Frontiers,12(2):11-21]
王成善,曹珂,黄永建.2009.沉积记录与白垩纪地球表层系统变化.地学前缘,16(5):1-14.[Wang C S,Cao K,Huang Y J.2009.Sedimentary record and Cretaceous earth surface System changes.Earth Science Frontiers,16(5):1-14]
王明振,吴朝东,房亚男,王陆新,李林林,陈榕,王军.2013.准噶尔盆地南缘坡缕石矿物学特征及古气候指示意义.岩石矿物学杂志,32(6):833-841.[Wang M Z,Wu C D,Fang Y N,Wang LX,Li L L,Chen R,Wang J.2013.Mineralogical characteristics of palygorskite in the southern margin of Junggar Basin and their implications for paleoclimate.Acta Petrologica et Mineralogica,32(6):833-841]
新疆维吾尔自治区地质矿产局.1999.新疆维吾尔自治区岩石地层.湖北武汉:中国地质大学出版社.[Bureau of Geology and Mineral Resources of Xinjiang Uygur Autonomous Region.1999.Lithostratigraphy of Xinjiang Uygur Autonomous Region.Wuhan of Hubei:China University of Geosciences Press]
许书堂,焦存礼,王敬缺.1998.伊犁盆地沉积岩颜色指数特征、盆地演化与有利勘探层系.勘探家,3(3):60-63.[Xu S T,Jiao CL,Wang J Q.1998.Sedimentary rock color index feature,basin evolution and favorable exploration strata in the Yili Basin.Petroleum Explorationist,3(3):60-63]
杨胜利,方小敏,李吉均,安芷生,陈诗越,福泽仁之.2001.表土颜色和气候定性至半定量关系研究.中国科学(D辑),31(增刊):175-181.[Yang S L,Fang X M,Li J J,An Z S,Chen S Y,Fortune Hitoshi.2001.Transformation functions of soil color and climate.Science in China(Series D),31(Suppl.):175-181]
雍天寿.1987.准噶尔盆地晚古生代-新生代岩相古地理.新疆石油地质,8(2):24-34.[Yong T S.1987.Junggar Basin Late Paleozoic-Cretaceous lithofacies and palaeogeography.Xinjiang Petroleum Geology,8(2):24-34]
An Z S,Kutzbach J E,Prell W L,Porter S C.2001.Evolution of Asian monsoons and phased up lift of the Himalaya-Tibetan plateau since Late Miocene times.Nature,411:62-66.
Avouac J P,Tapponnier P,Bai M,You H,Wang G.1993.Active thrusting and folding along the northern Tien Shan and Late Cenozoic rotation of the Tarim relative to Dzungaria and Kazakhstan.Journal of Geophysical Research:Solid Earth,98:6755-6804.
Bian W H,Hornung J,Liu Z H,Wang P J,Hinderer M.2010.Sedimentary and palaeoenvironmental evolution of the Junggar Basin,Xinjiang,Northwest China.Palaeogeography,Palaeoclimatology,Palaeoecology,90:175-186.
Charreau J,Chen Y,Gilder S,Dominguez S,Avouac J P,Sen S,Sun D J,Li Y A,Wang W M.2004.Magnetostratigraphy and rock magnetism of the Neogene Kuitun He section(northwest China):Implications for Late Cenozoic uplift of the Tianshan mountains.Earth and Planetary Science Letters,230:177-192.
Charreau J,Kent-Corson M L,Barrier R,Augier R,Ritts B D,Chen Y,France-Lannord C,Guilmette C.2012.A high-resolution stable isotopic record from the Junggar Basin(NW China):Implications for the paleotopographic evolution of the Tianshan Mountains.Earth and Planetary Science Letters,341-344:158-169.
Dewey J F,Shackelton R M,Chang C,Sun Y.1988.The tectonic evolution of the Tibetan Plateau.Phil.Trans.R.Soc.Lond.,A327:379-413.
Ding Z L,Yang S L,Hou S S,Chen Z,Liu T S.2001.Magnetostratigraphy and sedimentology of the Jingchuan red clay section and correlation of Tertiary eolian red clay sediments of the Chinese Loess Plateau.Journal of Geophysical Research:Solod Earth,106(B4):6399-6407.
Fang Y N,Wu C D,Wang Y Z,Wang L X,Guo Z J,Hu H W.2016.Stratigraphic and sedimentary characteristics of the Upper Jurassic-Lower Cretaceous strata in the Junggar Basin,Central Asia:Tectonic and climate implications.Journal of Asian Earth Sciences,129:294-308.
Frakes L A.1979.Climates throughout geologic time.Elsevier Scientific Pub.Co.10.1016/0025-3227(80)90114-0.
Guedes A,Ribeiro H,Valentim B,Noronha F.2009.Quantitative colour analysis of beach and dune sediments for forensic applications:APortuguese example.Forensic Science International,190:42-51.
Guo Z T,Ruddiman W F,Hao Q Z,Wu H B,Qiao Y S,Zhu R X,Peng SZ,Wei J J,Yuan B Y,Liu T S.2002.Onset of Asian desertification by 22 Myr ago inferred from loess deposits in China.Nature,416:159-163.
Haq B,Hardenbol J,Vail P.1988.Mesozoic and Cenozoic chronostratigraphy and cycles of sea-level change.SEPM Special Publication,42:71-108.
Ji J L,Pan L,Paul W,Jiang H C,Gao L,Ding Z L.2008.Episodic uplift of the Tianshan Mountains since the Late Oligocene constrained by magnetostratigraphy of the Jingou River section,in the southern margin of the Junggar Basin,China.Journal of Geophysical Research,113:B05102,doi:10.1029/2007JB005064.
Kent-Corson M L,Ritts B D,Zhuang G Z,Bovet P M,Graham S A,Chamberlain C P.2009.Stable isotopic constraints on the tectonic,topographic,and climatic evolution of the northern margin of the Tibetan Plateau.Earth and Planetary Science Letters,282(1-4):158-166.
Li J,Hu X M,Zhao K D,Cai Y F,Sun T.2016.Paleoceanographic evolution and chronostratigraphy of the Aptian Oceanic Anoxic Event 1a(OAE1a)to oceanic red bed 1(ORB1)in the Gorgo a Cerbara section(central Italy).Cretaceous Research,66:115-128.
Miller K G,Kominz M A,Browning J V,Wright J D,Mountain G S,Katz M E,Sugarman P J,Cramer B S,Christie-Blick N,Pekar S E.2005.The Phanerozoic record of global sea-level Change.Science,310:1293.
Myrow P M.1990.A new graph for understanding colors of mudrocks and shales.Journal of Geological Education,38:16-20.
Robertson A R.1977.The CIE 1976 color-difference formulae.Color research and Application,2(1):7-11.
Ruiz J F,Pereira J.2014.The colours of rock art:Analysis of colour recording and communication systems in rock art research.Journal of Archaeological Science,50:338-349.
Sun J M,Zhu R X,Bowler J.2004.Timing of the Tianshan Mountains uplift constrained by magnetostratigraphic analysis of molasse deposits.Earth and Planetary Science Letters,219(3-4):239-253.
Sun Y B,He L,Liang L J,An Z S.2011.Changing color of Chinese loess:Geochemical onstrint and paleoclimatic significance.Journal of Asian and Earth Sciences,40(6):1131-1138.
Tang Z H,Huang B C,Dong X X,Ji J L,Ding Z L.2012.Episodic uplift of the Tianshan Mountains since the Late Oligocene constrained by magnetostratigraphy of the Jingou River section,in the southern margin of the Junggar Basin,China.Journal of Geophysical Research,113,B05102.
Yang S L,Ding Z L.2003.Color reflectance of Chinese loess and its implications for climate gradient changes during the last two glacial-interglacial cycles.Geophysical Research Letters,30(20):2058.
Yu S,Chen W,Evans N J,Mcinnes B I A,Yin J Y,Sun J B,Li J,Zhang B.2014.Cenozoic uplift,exhumation and deformation in the north Kuqa Depression,China as constrained by(U-Th)/He thermochronometry.Tectonophysics,630:166-182.
Zheng G D,Fu B H,Duan Y,Wang Q,Matsuo M,Takano B.2004.Iron speciation related to color of Jurassic sedimentary rocks in Turpan Basin,northwest China.Journal of Radioanalytical and Nuclear Chemistry,261(2):421-427.
© 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 |