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塔里木早二叠世大火成岩省

, PP. 187-199

Keywords: 塔里木盆地,早二叠世,大火成岩省,时空特征,岩浆演化,地幔柱

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Abstract:

?塔里木早二叠世大火成岩省是继峨眉山大火成岩省之后在中国境内确认的又一个大火成岩省,是当前研究的热点和前沿问题.论文系统总结了塔里木大火成岩省近20年研究取得的成果,指出了下一步重点研究领域.塔里木大火成岩省火山岩的残余分布面积大于25万平方公里,最大残余厚度达780m,大规模玄武岩的喷出发生在290~288Ma期间,属于快速喷发的大火成岩省岩浆事件.塔里木大火成岩省中最为发育的玄武岩和辉绿岩岩墙的微量元素特征与OIB的特征相似,且以高钛型为主体;但在同位素特征上明显的可以分为两类,柯坪地区玄武岩具有负的εNd值,重稀土值相对较高,来自富集型地幔;塔北玄武岩和辉绿岩具有正的εNd值和相对低的重稀土值,来自亏损型地幔.早二叠世大规模地壳抬升、苦橄岩与大规模岩墙群发育和瓦基里塔格大型钒钛磁铁矿矿床都支持塔里木大火成岩省与地幔柱活动有关.塔里木大火成岩省与中亚地区广泛发育的二叠纪基性和超基性岩浆作用存在着时空联系,它们是代表了一次具有重要地球动力学意义的构造岩浆事件.论文指出了塔里木大火成岩省的深部地质过程、成矿作用、与地幔柱关系、与盆地环境变化和生命演化的关系及其大火成岩省的地球动力学意义等方面研究将是下一阶段的重点研究领域.

References

[1]  陈汉林, 杨树锋, 董传万, 等. 1997a. 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: 7-87
[2]  陈汉林, 杨树锋, 董传万, 等. 1997b. 塔里木盆地地质热事件研究. 科学通报, 42: 1-43
[3]  陈汉林, 杨树锋, 贾承造, 等. 1998. 塔里木盆地北部二叠纪中酸性火成岩带的厘定及其对塔北构造演化的新认识. 矿物学报, 18: 70-376
[4]  陈汉林, 杨树锋, 王清华, 等. 2006. 塔里木板块早-中二叠世玄武质岩浆作用的沉积响应. 中国地质, 33: 45-553
[5]  陈汉林, 杨树锋, 厉子龙, 等. 2009. 塔里木盆地二叠纪大火成岩省发育的时空特点. 新疆石油地质, 30: 79-182
[6]  陈咪咪, 田伟, 张自力. 2010. 塔里木二叠纪基性-中性-酸性岩浆岩的年代学及其地质意义. 岩石学报, 26: 559-572
[7]  贾承造. 1997. 中国塔里木盆地构造特征与油气, 北京: 石油工业出版社, 1997. 157-170
[8]  贾承造, 杨树锋, 陈汉林, 等. 2001. 特提斯北缘盆地群构造地质与天然气, 北京:石油工业出版社, 2001. 136
[9]  贾承造, 王良书, 魏国齐, 等. 2004. 塔里木盆地板块构造与大陆动力学. 北京: 石油工业出版社. 127-135
[10]  姜常义, 贾承造, 李良辰, 等. 2004a. 新疆麻扎尔塔格地区铁富集型高镁岩浆的源区. 地质学报, 78: 70-780
[11]  姜常义, 张蓬勃, 卢登蓉, 等. 2004b. 新疆塔里木板块西部瓦吉里塔格地区二叠纪超镁铁岩的岩石成因与岩浆源区. 岩石学报, 20: 3-44
[12]  姜常义, 张蓬勃, 卢登蓉, 等. 2004c. 柯坪玄武岩的岩石学、地球化学、Nd、Sr、Pb同位素组成与岩石成因. 地质论评, 50: 492-500
[13]  康玉柱. 2008. 新疆两大盆地石炭-二叠系火山岩特征与油气. 石油实验地质, 30: 321-327
[14]  李勇, 苏文, 孔屏. 2007. 塔里木盆地塔中-巴楚地区早二叠世岩浆岩的LA-ICP-MS锆石U-Pb年龄. 岩石学报, 23: 097-1107
[15]  厉子龙, 杨树锋, 陈汉林, 等. 2008, 塔西南玄武岩年代学和地球化学特征及其对二叠纪地幔柱岩浆演化的制约. 岩石学报, 2: 59-970
[16]  励音骐, 厉子龙, 孙亚莉, 等. 2010. 里木瓦吉里塔格超镁铁质隐爆角砾岩铂族元素和微量元素地球化学特征及其岩石成因探讨. 石学报, 26: 307-3317
[17]  吕修祥, 杨宁, 解启来, 等. 2005. 塔中地区深部流体对碳酸盐岩储层的改造作用. 石油与天然气地质, 2005, 26: 284-289
[18]  上官时迈, 田伟, 李献华, 等. 2011. 塔北哈拉哈塘流纹岩的离子探针锆石U-Pb年代学: 对塔里木溢流玄武岩主期喷发时代的约束. 北京大学学报(自然科学版), 47: 561-564
[19]  孙林华, 王岳军, 范蔚茗, 等. 2007. 新疆巴楚辉绿岩岩脉的岩石成因和大地构造意义. 岩石学报, 23: 1369-1380
[20]  杨树锋, 厉子龙, 陈汉林, 等. 2006. 塔里木二叠纪石英正长斑岩岩墙的发现及其构造意义. 岩石学报, 22: 1405-1412
[21]  王庭印, 刘金坤. 1991. 塔里木成盆期及裂谷作用初探. 见: 贾润胥, 主编. 中国塔里木盆地北部油气地质研究. 北京: 中国地质大学出版社. 115-124
[22]  杨树锋, 陈汉林, 董传万, 等. 1996. 塔里木盆地二叠纪正长岩的发现及其地球动力学意义. 地球化学, 25: 121-128
[23]  杨树锋, 陈汉林, 冀登武, 等. 2005. 塔里木盆地早-中二叠世岩浆作用过程及地球动力学. 高校地质学报, 11: 504-511
[24]  杨树锋, 余星, 陈汉林, 等. 2007. 塔里木盆地巴楚小海子二叠纪超基性脉岩的地球化学特征及其成因探讨. 岩石学报, 23: 1087-1096
[25]  于峻川, 莫宣学, 董国臣, 等. 2011. 塔里木北部二叠纪长英质火山岩年代学及地球化学特征. 岩石学报, 27: 2184-2194
[26]  余星. 2009. 塔里木早二叠世大火成岩省的岩浆演化与深部地质作用. 博士学位论文. 杭州: 浙江大学, 31-100
[27]  余星, 陈汉林, 杨树锋, 等. 2009. 塔里木盆地二叠纪玄武岩的地球化学特征及其与峨眉山大火成岩省的对比. 岩石学报, 25: 1492-1498
[28]  余星, 陈汉林, 杨树锋, 等. 2010. 新疆柯坪二叠纪层状玄武岩的发育特征及其地质意义, 地层学杂志, 34: 127-134
[29]  张传林, 周刚, 王洪燕, 等. 2010. 塔里木和中亚造山带西段二叠纪大火成岩省的两类地幔源区. 地质通报, 29: 779-794
[30]  张达玉, 周涛发, 袁峰, 等. 2010. 塔里木柯坪地区库普库兹曼组玄武岩锆石LA-ICP-MS年代学、Hf同位素特征及其意义. 岩石学报, 26: 963-974
[31]  张洪安, 李曰俊, 吴根耀, 等. 2009. 塔里木盆地二叠纪火成岩的同位素年代学. 岩石学报, 44: 137-158
[32]  周黎霞, 胡世玲, 王利刚, 等. 2010. 塔里木盆地西北缘皮羌辉长岩体的时代讨论. 地质科学, 45: 1057-1065
[33]  朱毅秀, 金之钧, 林畅松, 等. 2005. 塔里木盆地塔中地区早二叠世岩浆岩及油气成藏关系. 石油实验地质, 27: 50-54
[34]  Ali J R, Thompson G M, Zhou M F, et al. 2005. Emeishan large igneous province, SW China. Lithos, 79:475-489
[35]  Campbell I H. 2002. Identification of ancient mantle plumes. Mantle plumes: Their identification through time. Geol Soc Am, 352: 5-22
[36]  Chung S L, Jahn B M. 1995. Plume-lithosphere interaction in generation of the Emeishan flood basalts at the Permian-Triassic boundary. Geology, 23:89-892
[37]  Courtillot V, Jaeger J J, Yang Z, et al. 1996. The influence of continental flood basalts on mass extinctions: Where do we stand? In: Ryder G, Fastovsky D, Gartner S, eds. The Cretaceous-Tertiary Event and Other Catastrophes in Earth History. Geol Soc Am, 307: 513-525
[38]  Courtillot V, Jaupart C, Manighetti I, et al. 1999. On causal links between flood basalts and continental breakup. Earth Planet Sci Lett, 166: 177-195
[39]  Courtillot V, Davaille A, Besse J, et al. 2003. Three distinct types of hotspots in the Earth''s mantle. Earth Planet Sci Lett, 205: 295-308
[40]  Ernst R E, Buchan K L. 2003. Recognizing mantle plumes in the geological record. Annu Rev Earth Planet Sci, 31: 469-523
[41]  He B, Xu Y G, Chung S L, et al. 2003. Sedimentary evidence for a rapid, kilometer scale crustal doming prior to the eruption of the Emeishan flood basalts. Earth Planet Sci Lett, 213: 391-405
[42]  Li Y Q, Li Z L, Chen H L, et al. 2012. Mineral characteristics and metallogenesis of the Wajilitag layered mafic-ultramafic intrusion and associated Fe-Ti-V oxide deposit in the Tarim large igneous province, northwest China. J Asian Earth Sci, 49: 161-174
[43]  Li Z L, Chen H L, Song B, et al. 2011. Temporal evolution of the Permian large igneous province in Tarim Basin in northwestern China. J Asian Earth Scis, 42: 917-927
[44]  Li Z L, Li Y Q, Chen H L, et al. 2012. Hf isotopic characterisitcs of the Tarim Permian large igneous province rocks of NW China: Implication for the magmatic source and evolution. J Asian Earth Sci, 49: 191-202
[45]  Naldertt A J. 1999. World-class Ni-Cu-PGE deposits: Key factors in their genesis. Miner Depos, 34: 227-240
[46]  Olsen P E, Koeberl C, Huber H, et al. 2002. Continental Triassic-Jurassic boundary in central Pangea: Recent pregresss and discusssion of an Ir anomaly. In: Koeberl C, MacLeod K G, eds. Catastrophic Events and Mass Extinctions: Impacts and Beyond. Geol Soc Am, 356: 505-522
[47]  Pirajno F. 2000. Ore Deposi ts and Mant le Plumes. Dordrecht, Net herland: Kluwer Acad, 556
[48]  Pirajno F, Mao J W, Zhang Z C, et al. 2008. The association of mafic-ultramafic intrusions and A-type magmatism in the Tian Shan and Altay orogens, NW China: Implications for geodynamic evolution and potential for the discovery of new ore deposits. J Asian Earth Sci, 32: 165-183
[49]  Pirajno F, Ernst R E, Borisenko A S, et al. 2009. Intraplate magmatism in Central Asia and China and associated metallogeny. Ore Geol Rev, 35: 114-136
[50]  Qin K Z, Su B X, Sakyi P A, et al. 2011. SIMS ziron U-Pb geochronology and Sr-Nd isotopes of Ni-Cu bearing mafic-ultramafic intrusions in eastern Tianshan and Beishan in correlation with flood basalts in Tarim basin (NW China): Constraints on a ca. 280 Ma mantle plume. Am J Sci, 311: 237-260
[51]  Stothers R B, Rampino M R. 1990. Periodicity in flood basalts, mass extinctions, and impacts: A statistical review and a model. Geol Soc Am, 247: 9-18
[52]  Tian W, Campbell I H, Allen CM, et al. 2010. The Tarim picrite-basalt-rhyolite suite, a Permian flood basalt from northwest China with contrasting rhyolites produced by fractional crystallization and anatexis. Contrib Mineral Petrol, 160: 407-425
[53]  Turner S, Hawkesworth C J, Gallagher K. 1996. Mantle plumes, flood basalts, and thermal models for melt generation beneath continents: Assessment of a conductive heating model and application to the Parana. J Geophys Res, 101: 11503-11518
[54]  Wignall P B. 2001. Large igneous provinces and mass extinctions. Earth-Sci Rev, 53: 1-33
[55]  Windley B F, Alexeiev D, Xiao W J, et al. 2007. Tectonic models for accretion of the Central Asian Orogenic Belt. J Geol Soc, 164: 31-47
[56]  Xia L Q, Xu X Y, Li X M, et al. 2012. Reassessment of petrogenesis of Carboniferous-Early Permian rift-related volcanic rocks in the Chinese Tianshan and its neighboring areas. Geosci Front, 3: 445-471
[57]  Xiao L, Xu Y G, Chung S L, et al. 2003. Chemostratigraphic correlation of Upper Permian lavas from Yunnan Province, China: Extent of the Emeishan large igneous province. Int Geol Rev, 45: 753-766
[58]  Xiao L, Xu Y G, Mei H J, et al. 2004. Distinct mantle sources of low-Ti and high-Ti basalts from the western Emeishan large igneous province, SW China: implications for plume-lithosphere interaction. Earth Planet Sci Lett, 228: 525-546
[59]  Xu Y G, Chung S L, Jahn B M, et al. 2001. Petrologic and geochemical constraints on the petrogenesis of Permian-Triassic Emeishan flood basalts in southwestern China. Lithos, 58: 145-168
[60]  Xu Y G, He B, Chung S L, et al. 2004. Geologic, geochemical, and geophysical consequences of plume involvement in the Emeishan flood-basalt province. Geology, 32: 917-920
[61]  Yang S F, Li Z L, Chen H L, et al. 2006. 40Ar-39Ar dating of basalts from Tarim Basin, NW China and its implication to a Permian thermal tectonic event. J Zhejiang Univ, 7(Supp II): 170-174
[62]  Yang S F, Li Z L, Chen H L, et al. 2007. Discovery of Permian bimodal dyke: Geochemistry and implications for tectonic evolution related to the last major tectono-thermal event in Tarim Basin, NW China. Gondwana Res, 12: 113-120
[63]  Yu X, Yang S F, Chen H L, et al. 2011. Permian flood basalts from the Tarim Basin, Northwest China: SHRIMP zircon U-Pb dating and geochemical characteristics. Gondwana Res, 20: 485-497
[64]  Zhang C L, Li X H, Li Z X, et al. 2008. A Permian layered intrusive complex in the Western Tarim Block, northwestern China: Product of a ca. 275 Ma mantle plume? J Geol, 116: 269-287
[65]  Zhang C L, Li Z X, Li X H, et al. 2010. A Permian large igneous province in Tarim and Central Asian orogenic belt, NW China: Results of a ca. 275 Ma mantle plume? Soc Am Bull, 122: 2020-2040
[66]  Zhang Y T, Liu J Q, Guo Z F. 2010. Permian basaltic rocks in the Tarim basin, NW China: Implications for plume-lithosphere interaction. Gondwana Res, 18: 596-610
[67]  Zhou M F, Malpas J, Song X Y, et al. 2002. A temporal link between the Emeishan large igneous province (SW China) and the end-Guadalupian mass extinction. Earth Planet Sci Lett, 196: 113-122
[68]  Zhou M F, Zhao J H, Qi L, et al. 2006. Zircon U-Pb geochronology and elemental and Sr-Nd isotope geochemistry of Permian mafic rocks in the Funing area, SW China. Contrib Mineral Petrol, 151: 1-19
[69]  Zhou M F, Zhao J H, Jiang C Y, et al. 2009. OIB-like, heterogeneous mantle sources of Permian basaltic magmatism in the western Tarim basin, NW China: Implications for a possible Permian large igneous province. Lithos, 113: 583-594

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