房山变质核杂岩基底拆离断层韧性剪切变形构造及环境分析

姚丽景; 颜丹平; 胡玲

Volume 32 Issue 3

May 2007

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YAO Li-jing, YAN Dan-ping, HU Ling, 2007. Structure Style and Temperature-Pressure Estimation of the Detachment Fault Zone around Fangshan Dome, Western Hills of Beijing. Earth Science, 32(3): 357-365.

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YAO Li-jing, YAN Dan-ping, HU Ling, 2007. Structure Style and Temperature-Pressure Estimation of the Detachment Fault Zone around Fangshan Dome, Western Hills of Beijing. Earth Science, 32(3): 357-365.

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Structure Style and Temperature-Pressure Estimation of the Detachment Fault Zone around Fangshan Dome, Western Hills of Beijing

State Key Laboratory o f Geological Processes and Mineral Resources, China University o f Geosciences, Beijing 100083, China

Received Date: 2006-09-08
Publish Date: 2007-05-25

Abstract

Abstract

The basement ductile shear zone of the Fangshan extensional dome separates the Archean Guandi complex from various cover strata in southern and northern margins of Fangshan pluton.This ductile shear zone is composed of the ductilely deformed fabrics with an SE-ward kinematic, which can be deduced from rock and mineral deformations, including faultage offect and so on, on both macroscopic and microcosmic scales.Typical regional-dynamic metamorphic mineral pair hornblende-plagioclase and high pressure mineral muscovite with high Si are common and identified within the ductile shear zone.EPMA analysis of the mineral pair gives a metamorphic condition of T=492-555 ℃ and p=0.33 GPa, which indicates a metamorphic grade of lower-amphibolite facies and a depth of around 12.9 km estimated following a normal lithostatic pressure.Field evidences, including that Fangshan pluton intruded the Archean Guandi complex and the ductile shear zone, lots of gneissic xenolithes within the Fangshan pluton, and that a lot of quartz monzonite-diorite intruded along the fabric of the ductile shear zone, support that the ductile shear zone was formed before Fangshan pluton, and likely to be simultaneous with the formation of the Fangshan detachment zone of the extensional dome.
- Fangshan detachment zone,
- ductile shear zone,
- rectangle quartz ribbons,
- hornblende-plagioclase mineral pair,
- muscovite

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References(47)

References

Hammarstrom, J.M., Zen, E.A., 1986. Alminum in hornblende: An empirica ligneous geobarometer. American Mineralogist, 71: 1297-1313.

He, B., Xu, Y.G., Wang, Y.M., et al., 2005. Magmatic diapir of Fangshan pluton in the Western Hills, Beijing and its geological significance. Earth Science-Journal of China University of Geosciences, 30 (3) : 298-307 (in Chinese with English abstract).

Holland, T., Blundy, J., 1994. Non-ideal interactions in calcic amphiboles and their bearing on amphibole-plagioclase thermometry. Contrib. Mineral. Petrol., 116: 433-447. doi: 10.1007/BF00310910

Hu, L., 1998. Introduction to microstructural geology. Geological Publishing House, Beijing (in Chinese).

Johnson, M.C., Rutherford, M.J., 1988. Experimental calibration of an aluminium-in-hornblende geobarometer applicable to calk-alkaline rocks. EOS Transactions, 69 (44) : 1511-1988.

Johnson, M.C., Rutherford, M.J., 1989a. Experimentally determined conditions in the Fish canyon tuff, Colorado, magma chamber. Petrology, 30 (3) : 711-737. doi: 10.1093/petrology/30.3.711

Johnson, M.C., Rutherford, M.J., 1989b. Experimental calibration of the aluminum-in-hornblende geobarometer with application of Long Valley caldera (California) volcanic rocks. Geology, 17 (9) : 837-841. https://pubs.geoscienceworld.org/gsa/geology/article-abstract/17/9/837/204999/Experimental-calibration-of-the-aluminum-in

Li, L.R., Wang, C.Z., 1996. Classification of multi-grain quartz ribbons in mylonites and their development conditions. Journal of Guilin Institute of Technology, 16 (3) : 224-231 (in Chinese with English abstract).

Lin, Z.Y., Liu, J.L., Fang, J.Y., 2002. Mechanisms of deformation and recrystallization of quartz during extension. World Geology, 21 (4) : 321-326 (in Chinese with English abstract).

Liu, G.H., Wu, J.S., 1977. Metamorphic rocks and metamorphic zones around Fangshan pluton. The Study of Geological Mineral Resources, (3) : 159-198 (in Chinese with English abstract). https://www.sciencedirect.com/science/article/pii/S0191814109000856

Liu, Z.H., Li, D.D., 1999. Recrystallization and its microfabrics in mylonite. Jilin Geology, 18 (4) : 32-37 (in Chinese with English abstract).

Ma, H.W., 2001. Introduction to crystallography thermodynamics. High Education Press, Beijing, 93-102 (in Chinese).

Massone, H.J., Scbreyer, W., 1989. Stability field of the high-pressure assemblage talc + phengite and two new phengite barometers. Eur. J. Mineral, (1) : 391-410. https://pubs.geoscienceworld.org/eurjmin/article-abstract/1/3/391/61460/Stability-field-of-the-high-pressure-assemblage

Shan, W.L., Fu, Z.R., 1987. A preliminary analysis of the horizontal laminar shear-flow structure in the Western Hills of Beijing. Earth Science-Journal of Wuhan College of Geology, 12 (2) : 113-120 (in Chinese with English abstract).

Shan, W.L., Wang, F.Z., Fu, Z.R., et al., 1989. On the tectonic evolution of cover rocks in the southern part of Western Hills of Beijing. Earth Science-Journal of China University of Geosciences, 14 (1) : 37-50 (in Chinese with English abstract).

Song, H.L., 1987. A primary analysis on the tectonic sequence in the southern part of the Western Hills of Beijing. Earth Science-Journal of Wuhan College of Geology, 12 (1) : 15-20 (in Chinese with English abstract).

Song, H.L., 1996. Characteristics of Fangshan metamorphic core complex, Beijing and a discussion about its origin. Geoscience, 10 (2) : 149-158 (in Chinese with English abstract).

Song, H.L., 2002. Some characteristics of metamorphic core complexes. Geological Bulletin of China, 21 (4-5) : 194-197 (in Chinese with English abstract).

Song, H.L., Ge, M.C., 1984. The Indosinian movement in the Western Hills of Beijing discussed in the light of the structural characteristics. Geological Review, 30 (1) : 77-80 (in Chinese with English abstract).

Song, H.L., He, B., Zheng, Z.S., et al., 1990. Denudational fault of West-Hill, Beijing. In: Zhang, J.S., Shan, W.L., eds., The geological study of Western Hills of Beijing. China University of Geosciences Press, Wuhan, 19-28 (in Chinese).

Song, H.L., Shan, W.L., 1987. Denudational fault, intraplate subhorizontal shear zone and extensional tectonics. Earth Science-Journal of Wuhan College of Geology, 12 (5) : 535-541 (in chinese with English abstract).

Su, S.G., Lai, X.Y., 1994. A review of new geobarometers applicable to high-pressure metamorphism. Geological Science and Technology Information, 13 (2) : 91-97 (in Chinese with English abstract).

Xiao, Q.H., 1985. The microstructure of mylonites and their origin-A review. In: Structural Geology Reviews, (5) : 203-216. Geological Publishing House, Beijing (in Chinese).

Xu, Z.Q., Wang, G.F., Fu, Z.K., 1985. Ductile decollement shear zone in the Western Hills of Beijing. Bulletin of the Chinese Academy of Geological Sciences, (11) : 37-52 (in Chinese with English abstract).

Yan, D.P., Zhou, M.F., Song, H.L., et al., 2005. A geochronological constraint to the Guandi complex, Western Hills of Beijing, and its implications for the tectonic evolution. Earth Science Frontiers, 12 (2) : 332-337 (in Chinese with English abstract).

Yan, D.P., Zhou, M.F., Song, H.L., et al., 2006. Mesozoic extensional structures of the Fangshan tectonic dome and their subsequent reworking during collisional of accretion of the North China block. Journal of the Geological Society, London, 163: 127-142. doi: 10.1144/0016-764904-154

Zhao, S.R., Bian, Q.J., Ling, Q.C., 2004. Crystallography and mineralogy. High Education Press, Beijing, 376 (in Chinese).

何斌, 徐义刚, 王雅玫, 等, 2005. 北京房山岩体岩浆底劈构造及地质意义. 地球科学——中国地质大学学报, 30 (3) : 298-307. https://www.cnki.com.cn/Article/CJFDTOTAL-DQKX200503005.htm

胡玲, 1998. 显微构造地质学概论. 北京: 地质出版社.

李兰荣, 王春增, 1996. 糜棱岩中多晶石英条带的类型及形成条件. 桂林工学院学报, 16 (3) : 224-231. https://www.cnki.com.cn/Article/CJFDTOTAL-GLGX603.003.htm

蔺志永, 刘俊来, 方建勇, 2002. 伸展作用过程中石英变形与重结晶的微观机制. 世界地质, 21 (4) : 321-326. doi: 10.3969/j.issn.1004-5589.2002.04.002

刘国惠, 伍家善, 1977. 北京房山岩体围岩的变质岩石学和变质带. 地质矿产研究, (3) : 159-198.

刘正宏, 李殿东, 1999. 糜棱岩的重结晶作用及其显微组构. 吉林地质, 18 (4) : 32-37. https://www.cnki.com.cn/Article/CJFDTOTAL-JLDZ199904004.htm

马鸿文, 2001. 结晶岩热力学概论. 北京: 高等教育出版社, 93-102.

单文琅, 傅昭仁, 1987. 北京西山水平分层剪切流变构造初探. 地球科学——武汉地质学院学报, 12 (2) : 113-120. https://www.cnki.com.cn/Article/CJFDTOTAL-DQKX198702000.htm

单文琅, 王方正, 傅昭仁, 等, 1989. 论北京西山南部的盖层构造演化. 地球科学——中国地质大学学报, 14 (1) : 37-50. https://www.cnki.com.cn/Article/CJFDTOTAL-DQKX198901007.htm

宋鸿林, 1996. 北京房山变质核杂岩的基本特征及成因探讨. 现代地质, 10 (2) : 149-158. https://www.cnki.com.cn/Article/CJFDTOTAL-XDDZ602.001.htm

宋鸿林, 1987. 北京西山南部构造序列初探. 地球科学——武汉地质学院学报, 12 (1) : 15-20. https://www.cnki.com.cn/Article/CJFDTOTAL-DQKX198701002.htm

宋鸿林, 2002. 关于变质核杂岩构造特征的几个问题. 地质通报, 21 (4~5) : 194-197. https://www.cnki.com.cn/Article/CJFDTOTAL-ZQYD2002Z1001.htm

宋鸿林, 葛梦春, 1984. 从构造特征论北京西山的印支运动. 地质论评, 30 (1) : 77-80. doi: 10.3321/j.issn:0371-5736.1984.01.011

宋鸿林, 何斌, 郑在胜, 等, 1990. 北京西山的剥离断层. 见: 张吉顺, 单文琅主编, 北京西山地质研究. 武汉: 中国地质大学出版社, 19-28.

宋鸿林, 单文琅, 1987. 剥离断层、板块内近水平的剪切带与伸展构造. 地球科学——武汉地质学院学报, 12 (5) : 535-541. https://www.cnki.com.cn/Article/CJFDTOTAL-DQKX198705013.htm

苏尚国, 赖兴运, 1994. 高压变质作用压力估算的热力学方法. 地质科技情报, 13 (2) : 91-97. https://www.cnki.com.cn/Article/CJFDTOTAL-DZKQ402.019.htm

肖庆辉, 1985. 糜棱岩的显微构造和成因(评述). 见: 构造地质论丛, (5) : 203-216. 北京: 地质出版社.

许志琴, 王国方, 符振康, 1985. 北京西山的深部韧性滑脱剪切带. 中国地质科学院院报, (11) : 37-52. https://www.cnki.com.cn/Article/CJFDTOTAL-DQXB198500002.htm

颜丹平, 周美夫, 宋鸿林, 等, 2005. 北京西山官地杂岩的形成时代及构造意义. 地学前缘, 12 (2) : 332-337. doi: 10.3321/j.issn:1005-2321.2005.02.035

赵珊茸, 边秋娟, 凌其聪, 2004. 结晶学及矿物学. 北京: 高等教育出版社, 376.

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Structure Style and Temperature-Pressure Estimation of the Detachment Fault Zone around Fangshan Dome, Western Hills of Beijing

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