札达盆地碎屑裂变径迹揭示的盆山耦合过程

孟艳宁; 王国灿; 张克信; 王岸

doi:10.3799/dqkx.2010.089

Volume 35 Issue 5

Sep. 2010

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Article Navigation > Earth Science > 2010 > 35(5): 747-758

MENG Yan-ning, WANG Guo-can, ZHANG Ke-xin, WANG An, 2010. Coupling Process of Sedimentary Basin-Orogenic Belt Induced by Detrital Fission Track Ages of Zanda Basin. Earth Science, 35(5): 747-758. doi: 10.3799/dqkx.2010.089

Citation:

MENG Yan-ning, WANG Guo-can, ZHANG Ke-xin, WANG An, 2010. Coupling Process of Sedimentary Basin-Orogenic Belt Induced by Detrital Fission Track Ages of Zanda Basin. Earth Science, 35(5): 747-758. doi: 10.3799/dqkx.2010.089

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Coupling Process of Sedimentary Basin-Orogenic Belt Induced by Detrital Fission Track Ages of Zanda Basin

doi: 10.3799/dqkx.2010.089

MENG Yan-ning^{1, 2},
WANG Guo-can^{1, 2
,
,},
ZHANG Ke-xin^{2, 3},
WANG An^{1, 2}

1.
State Key Laboratory of Geological Process and Mineral Resources, China University of Geosciences, Wuhan 430074, China
2.
Faculty of Earth Sciences, China University of Geosciences, Wuhan 430074, China
3.
Key Laboratory of Biogeology and Environmental Geology of Ministry of Education, China University of Geosciences, Wuhan 430074, China

Received Date: 2010-05-31
Publish Date: 2010-09-01

Abstract

Abstract

Zanda basin, formed in 9.5 Ma, is a Cenozoic sedimentary basin which lies in the converging range between the Himalaya tectonic belt and Karakorum tectonic belt. The Neogene strata in the basin are integrated, continuous and horizontal, showing a steady tectonic condition since Miocene. Analysis of sedimentary section indicates that ancient flow direction is northwest to southeast, while the modern flow direction of river—Xiangquan River is southeast to northwest, opposite to the ancient flow direction. Analysis of sendimentary construction and the composition of gravel displays that the sedimentary source is Ayila Rijyu northwest of Zanda basin. P1, P2 peak ages of Zanda basin are 12.6—15.3 Ma and 19.8—22.2 Ma respectively, which is consistent with the thermal event age of Ayila Rijyu. P1, P2 are of static peak ages, reflecting the rapid cooling event such as normal faulting based on the DZFT research of lag time and depositional time by Bernet and Garver. It is found by thermal history analysis of zircon and apatite fission track that the cooling rate of source area is 15.4 ℃/Ma at 32.6—9.5 Ma, and there was a rapid uplift and exhumation at the same time in the source region at 3.6—1.4 Ma reflected by zircon and apatite fission track ages. P1, P2 peak ages of modern river zircon samples of Karakurom belt are 10.5—10.8 Ma and 27.7—30.9 Ma respectively, showing the thermal events of Ayila Rijyu. Comparing the FT ages and depositional information of Zanda basin and orogenetic belt, it is shown that Zanda basin is Cenozoic sedimentary basin determined by southeast of Karakorum fault; Zanda basin and Ayila Rijyu Moutain are a typical coupling process by identical FT thermochronology structure.
- Zanda basin,
- fission track,
- Ayila Rijyu Moutain,
- Karakorum fault

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References(67)

References

Bernet, M., Brandon, T.M., Garver, J.I., et al., 2002. Determining the zircon fission-track closure temperature; a zero-damage model for fission-track annealing in zircon. Abstracts with Programs—Geological Society of America. 34(5): 18. http://www.mendeley.com/research/determining-zircon-fissiontrack-closure-temperature/

Bernet, M., Garver, J.I., 2005. Fission-track analysis of detrital zircon. Reviews in Mineralogy and Geochemistry, 58(1): 205-237. doi: 10.2138/rmg.2005.58.8

Brandon, M.T., Roden-Tice, M.K., Garver, J.I., 1998. Late Cenozoic exhumation of the Cascadia accretionary wedge in the Olympic Mountains, Northwest Washington State. Geological Society of America, 110(8): 985-1009. doi:10.1130/0016-7606(1998)110<0985:LCEOTC>2.3.CO

Chen, Y., Chen, S.Y., Zhang, P.F., et al., 2008. Discussion on research methods of paleocurrent direction. Fault-Block Oil & Gas Field, 15(1): 37-40 (in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-DKYT200801015.htm

Franck, V., Philippe, H.L., Jean-Louis, P., et al., 2008. New U-Th/Pb constraints on timing of shearing and long-term slip-rate on the Karakorum fault. Tectonics, 27: 1-33. doi: 10.1029/2007TC002184

Gao, X., 2006. The environment and evolution of Zhada basin, Tibet (Dissertation). China University of Geosciences, Beijing, 46-52 (in Chinese).

Guo, T.Y., Liang, D.Y., Zhang, Y.Z., et al., 1991. Ali, Tibet, geology. China University of Geosciences Press, Wuhan, 103-104 (in Chinese).

Hurford, A.J., 1986. Cooling and uplift patterns in the Lepontine Alps, South Central Switzerland and an age of vertical movement on the Insubric fault line. Contributions to Mineralogy and Petrology, 92(4): 413-427. doi: 10.1007/BF00374424

Li, B.Y., Wang, F.B., Zhang, Q.S., et al, 1983. Quaternary geology of Tibet. Science Press, Beijing, 15-40 (in Chinese).

Li, H.B., Franck, V., Xu, Z.Q., et al., 2006. Deformation and tectonic evolution of the Karakorum fault, western Tibet. Chinese Geology, 33(2): 239-255 (in Chinese with English abstract).

Li, H.B., Franck, V., Liu, D.Y., et al., 2007. Forming age of Karakorum: age constrains of zircon SHRIMP U-Pb. Chinese Science Bulletin, 52(4): 438-447 (in Chinese). doi: 10.1360/csb2007-52-4-438

Matte, P., Tapponnier, P., Arnaud, N., et al., 1996. Tectonics of western Tibet, between the Tarim and the Indus. Earth Planet. Sci. Lett. , 142: 311-330. doi: 10.1016/0012-821X(96)00086-6

Meng, X.G., Zhu, D.G., Shao, Z.G., et al., 2004. Discovery of rhinoceros fossils in the Pliocene in the Zanda basin, Ngari, Tibet. Geological Bulletin of China, 23(5): 609-612 (in Chinese with English abstract).

Meng, X.G., Zhu, D.G., Shao, Z.G., et al., 2006. The basic characteristics and evolution of the geological structures in the Zhada basin, Ali, Tibet. Earth Science Frontiers, 13(4): 160-167 (in Chinese with English abstract).

Murphy, M.A., Yin, A., Kapp, P., et al., 2000. Southward propagation of the Karakoram fault system, Southwest Tibet: timing and magnitude of slip. Geology, 28(5): 451-454. doi:10.1130/0091-7613(2000)28<451:SPOTKF>2.0.CO;2

Murphy, M.A., Yin, A., Kapp, P., et al., 2002. Structural evolution of the Gurla Mandhata detachement system, Southwest Tibet: implications for the eastward extent of the Karakoram fault system. Geol. Soc. Am. Bull., 114: 428-447. doi: 10.1130/0016-7606(2002)114<0428:SEOTGM>2.0.CO;2

Naeser, C.W., 1979. Thermal history of sedimentary basins: fission-track dating of subsurface rocks. In: Scholle, P.A., Schluger, P.R., ed., Aspect of diagenesis. SEPM Spec. Publ., 26: 109-112.

Pei, J.L., Sun, Z.M., Wang, X.S., et al., 2009. Evidence for Tibetan plateau uplift in Qaidam basin before Eocene-Oligocene boundary and its climatic implications. Journal of Earth Science, 20(2): 430-437. doi: 10.1007/s12583-009-0035-y

Phillips, R.J., Parrish, R.R., Searle, M.P., 1991. Age constraints on ductile deformation and long-term slip rates along the Karakoram Moutains Map 2538. John Wiley and Sons, Chichester.

Qian, F., 1990. Paleomagnetic methods used in Tibet since the Pliocene Ali, a preliminary study of horizontal movement. In: Li, G.C., ed., Himalayan tectonic evolution of the lithosphere—Tibet geophysical proceedings. Geological Publishing House, Beijing, 198-206 (in Chinese).

Qian, F., 1999. Study on magnetostratigraphy in Qinghai-Tibetan plateau in Late Cenozoic. Journal of Geomechanics, 5(4): 22-34 (in Chinese with English abstract).

Rolland, Y., Mahéo, G., Pécher, A., et al., 2009. Syn-kinematic emplacement of the Pangong metamorphic and magmatic complex along the Karakorum fault(N Ladakh). Journal of Asian Earth Sciences, 34: 10-25. doi: 10.1016/j.jseaes.2008.03.009

Searle, M.P., Weinberg, R.F., Dunlap, W.J., 1998. Transpressional tectonics along the Karakoram fault zone, northern Ladakh: constraints on Tibetan extrusion. Geol. Soc. London Spec. Pub., 135: 307-326. doi: 10.1144/GSL.SP.1998.135.01.20

Shao, Z.G., Meng, X.G., Zhu, D.G., et al., 2005. Active faults in the Zhada basin of the Ngari area, Tibet, China. Geological Bulletin of China, 24(7): 625-629 (in Chinese with English abstract).

Shao, Z.G., Meng, X.G., Yang, C.B., et al., 2006. Formation mechanism of seesaw type in Zanda basin, Ngari, Xizang (Tibet). Geological Review, 52(2): 215-218 (in Chinese with English abstract).

Wang, A., Wang, G.C., Zhang, K.X., et al., 2009. Late Neogene mountain building of eastern Kunlun orogen: constrained by DEM analysis. Journal of Earth Science, 20(2): 391-400. doi: 10.1007/s12583-009-0032-1

Wang, G.C., 2002. A new approach to determine the exhumation history of the sediment provenance: detrital zircon and apatite fission-track thermochronology. Geological Science and Technology Information, 21(4): 35-40 (in Chinese with English abstract). http://www.en.cnki.com.cn/Article_en/CJFDTOTAL-DZKQ200204007.htm

Wang, J., Zhu, D.G., Meng, X.G., et al., 2006. Features of the change in Pliocene depositional environment at the Guge Formation section in the Zanda basin, Tibet. Geology in China, 33(5): 1005-1012 (in Chinese with English abstract).

Wang, S.F., Blisniuk, P., Kempf, O., et al., 2008a. The basin-range system along the south segment of Karakorum fault zone, Tibet. Int. Geol. Rev., 50(2): 121-134. doi: 10.2747/0020-6814.50.2.121

Wang, S.F., Zhang, W.L., Fang, X.M., et al., 2008b. Magnetic characteristics and tectonic significance of Zanda basin, Tibet. Chinese Science Bulletin, 53(6): 676-683 (in Chinese). doi: 10.1360/csb2008-53-6-676

Wang, W.L., Zhang, J.J., Zhang, B., 2004. Structural and sendimentary features in Zanda basin of Tibet. Acta Scientiarum Naturalium, 40(6): 872-878 (in Chinese with English abstract).

Xia, D.X., Liu, S.K., 1997. Tibet Autonomous Region lithostratigraphy. China University of Geosciences Press, Wuhan, 239-240(in Chinese).

Zhang, J.J., 2007. A review on the extensional structures in the northern Himalaya and southern Tibet. Geological Bulletin of China, 26(6): 639-649 (in Chinese with English abstract).

Zhang, J.J., Guo, L., 2007. Structure and geochronology of the southern Xainza-Dinggye rift and its relationship to the South Tibetan detachment system. Journal of Asian Earth Sciences, 29: 722-736. doi: 10.1016/j.jseaes.2006.05.003

Zhang, K.X., Wang, G.C., Cao, K., et al., 2008. Main uplift events of Tibet in Cenozoic: sedimentary response and thermochronology record. Science in China (Ser. D), 38(12): 1575-1588 (in Chinese).

Zhang, Q.S., Wang, F.B., Ji, H.X., et al., 1981. Pliocene strata of Zanda basin, Tibet. Journal of Stratigraphy, 5(3): 216-220 (in Chinese).

Zhao, Z.Z., Li, Y.T., Ye, H.F., et al., 2001. Qinghai-Tibet plateau formation. Science Press, Beijing, 177-322 (in Chinese).

Zheng, D.W., Zhang, P.Z., Wan, J.L., et al, 2000. Detrital grain thermochronology—a potential method for research on coupling process between basin and mountain. Seismology and Geology, 22(B12): 25-36 (in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTotal-DZDZ2000S1005.htm

Zhou, Y., Ding, L., Deng, W.M., et al., 2000. Tectonic cyclothems in the Zanda basin and its significance. Chinese Journal of Geology, 35(3): 305-315 (in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-DZKX200003005.htm

Zhou, Y., Xu, R.H., Yan, Y.H., et al., 2001. Dating of the Karakorum strike-slip fault. Acta Geologica Sinica, 75(1): 10-18. http://d.wanfangdata.com.cn/Periodical/dzxb-e200101002

Zhu, D.G., Meng, X.G., Shao, Z.G., et al., 2006. The formation and evolution of Zhada basin in Tibet and the uplift of the Himalayas. Acta Geoscientica Sinica, 27(3): 193-200 (in Chinese with English abstract).

Zhu, D.G., Meng, X.G., Shao, Z.G., et al., 2007. Evolution of the paleovegetation, paleoenvironment and paleoclimate during Pliocene-Early Pleistocene in Zhada basin, Ali, Tibet. Acta Geologica Sinica, 81(3): 295-307(in Chinese with English abstract). http://www.researchgate.net/publication/285896181_Evolution_of_the_paleovegetation_paleoenvironment_and_paleoclimate_during_Pliocene-early_Pleistocene_in_Zhada_basin_Ali_Tibet

陈妍, 陈世悦, 张鹏飞, 等, 2008. 古流向的研究方法探讨. 断块油气田, 15(1): 37-40. https://www.cnki.com.cn/Article/CJFDTOTAL-DKYT200801015.htm

高雄, 2006. 西藏札达盆地形成环境及其发展演化(硕士学位论文). 北京: 中国地质大学, 46-52.

郭铁鹰, 梁定益, 张宜智, 等, 1991. 西藏阿里地质. 武汉: 中国地质大学出版社, 103-104.

李炳元, 王富葆, 张青松, 等, 1983. 西藏第四纪地质. 北京: 科学出版社, 15-40.

李海兵, Franck, V., 许志琴, 等, 2006. 喀喇昆仑断裂的变形特征及构造演化. 中国地质, 33(2): 239-255. doi: 10.3969/j.issn.1000-3657.2006.02.002

李海兵, Franck, V., 刘敦一, 等, 2007. 喀喇昆仑断裂的形成时代: 锆石SHRIMP U-Pb年龄的制约. 科学通报, 52(4): 438-447. doi: 10.3321/j.issn:0023-074X.2007.04.012

孟宪刚, 朱大岗, 邵兆刚, 等, 2004. 西藏阿里札达盆地上新统中犀类化石的发现及意义. 地质通报, 23(5): 609-612. doi: 10.3969/j.issn.1671-2552.2004.05.036

孟宪刚, 朱大岗, 邵兆刚, 等, 2006. 西藏阿里札达盆地地质构造的基本特征及其演化. 地学前缘, 13(4): 160-167. doi: 10.3321/j.issn:1005-2321.2006.04.013

钱方, 1990. 用古地磁方法对西藏阿里上新世以来水平运动的初步研究. 见: 李兴岑编, 喜马拉雅岩石圈构造演化-西藏地球物理论文集. 北京: 地质出版社, 198-206.

钱方, 1999. 青藏高原晚新生代磁性地层研究. 地质力学学报, 5(4): 22-34. https://www.cnki.com.cn/Article/CJFDTOTAL-DZLX199904002.htm

邵兆刚, 孟宪刚, 朱大岗, 等, 2005. 西藏阿里地区札达沉积盆地活动构造. 地质通报, 24(7): 625-629. doi: 10.3969/j.issn.1671-2552.2005.07.006

邵兆刚, 孟宪刚, 杨朝斌, 等, 2006. 西藏阿里札达盆地的"翘板式"形成机制. 地质论评, 52(2): 215-218. https://www.cnki.com.cn/Article/CJFDTOTAL-DZLP200602010.htm

王国灿, 2002. 沉积物源区剥露历史分析的一种新途径——碎屑锆石和磷灰石裂变径迹热年代学. 地质科技情报, 21(4): 35-40. https://www.cnki.com.cn/Article/CJFDTOTAL-DZKQ200204007.htm

王津, 朱大岗, 孟宪刚, 等, 2006. 西藏札达盆地古格组剖面沉积环境演化特征. 中国地质, 33(5): 1005-1012. doi: 10.3969/j.issn.1000-3657.2006.05.008

王世锋, 张伟林, 方小敏, 等, 2008b. 藏西南札达盆地磁性地层学特征及其构造意义. 科学通报, 53(6): 676-683. https://www.cnki.com.cn/Article/CJFDTOTAL-KXTB200806013.htm

王维亮, 张进江, 张波, 2004. 西藏札达盆地构造与沉积特征. 北京大学学报(自然科学报), 40(6): 872-878. https://www.cnki.com.cn/Article/CJFDTOTAL-BJDZ200406004.htm

夏代祥, 刘世坤, 1997. 西藏自治区岩石地层. 武汉: 中国地质大学出版社, 239-240.

张进江, 2007. 北喜马拉雅及藏南伸展构造综述. 地质通报, 26(6): 639-649. https://www.cnki.com.cn/Article/CJFDTOTAL-ZQYD200706003.htm

张克信, 王国灿, 曹凯, 等, 2008. 青藏高原新生代主要隆升事件: 沉积响应与热年代学记录. 中国科学(D辑), 38(12): 1575-1588. https://www.cnki.com.cn/Article/CJFDTOTAL-JDXK200812011.htm

张青松, 王富葆, 计宏祥, 等, 1981. 西藏札达盆地的上新世地层. 地层学杂志, 5(3): 216-220. https://www.cnki.com.cn/Article/CJFDTOTAL-DCXZ198103008.htm

赵政章, 李永铁, 叶和飞, 等, 2001. 青藏高原地层. 北京: 科学出版社, 177-322.

郑德文, 张培震, 万景林, 等, 2000. 碎屑颗粒热年代学——一种揭示盆山耦合过程的年代学方法. 地震地质, 22(B12): 25-36. https://www.cnki.com.cn/Article/CJFDTOTAL-DZDZ2000S1005.htm

周勇, 丁林, 邓万明, 等, 2000. 札达盆地构造旋回层及其地质意义. 地质科学, 35(3): 305-315. https://www.cnki.com.cn/Article/CJFDTOTAL-DZKX200003005.htm

朱大岗, 孟宪刚, 邵兆刚, 等, 2006. 西藏札达盆地形成演化与喜马拉雅山隆升. 地球学报, 27(3): 193-200. https://www.cnki.com.cn/Article/CJFDTOTAL-DQXB200603000.htm

朱大岗, 孟宪刚, 邵兆刚, 等, 2007. 西藏阿里札达盆地上新世-早更新世的古植被、古环境与古气候演化. 地质学报, 81(3): 295-307. https://www.cnki.com.cn/Article/CJFDTOTAL-DZXE200703001.htm

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Coupling Process of Sedimentary Basin-Orogenic Belt Induced by Detrital Fission Track Ages of Zanda Basin

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