CHARACTERISTICS OF PALEOTECTONIC STRESS FILED ON THE AILAOSHAN STRUCTURAL BELT
-
摘要:
通过野外对哀牢山构造带漠沙镇、戛洒镇两地的哀牢山群中的构造形迹和形变特征进行观察和记录，将哀牢山构造带的应力场初步划分为韧性和脆性两期，并通过对构造带中的各种小构造（片理、劈理、褶皱、构造透镜体、擦痕及节理等）进行构造解析，初步获得了哀牢山构造带中至少存在两期构造应力场，其主压应力方向：北东—南西和北西—南东向挤压，现今构造应力场继承了古构造应力场；最后结合前人研究成果，简要分析了哀牢山构造带两种不同构造应力场的动力来源，即可能与构造带所处的周边板块和深部流体挤压作用有重要联系。
Abstract:By observing and recording structural feature and deformation of the Ailaoshan Group in the field at Mosha and Jiasa, the stress filed shall be preliminarily divided into two stages: the ductile deformation and brittle deformation. Based on the structural analysis of the stress field for all sorts of small structures, such as schistosity, cleavage, fold, tectonic lens, scratch and the conjugated joints, etc. in the field, it reveals that there exists two tectonic stress fields in the Ailaoshan structural belts, with main stress orientations of NE-SW and NW-SE compressions. The present stress filed sustains the paleotectonic stress filed. Combing with the previous research results, the dynamic sources of two different tectonic stress fields on the Ailaoshan belt are studied briefly, which may be critically linked to its peripheral plates and deep fluid extrusion.
-
Key words:
- Ailaoshan /
- structural belt /
- tectonic stress filed /
- dynamics
-
-
[1] 刘俊来, 唐渊, 宋志杰, 等.滇西哀牢山构造带:结构与演化[J].吉林大学学报:地球科学版, 2011, 41(5):1295~1303. http://www.cnki.com.cn/Article/CJFDTOTAL-CCDZ201105004.htm
LIU Jun-lai, TANG Yuan, SONG Zhi-jie, et al. The Ailaoshan belt in western Yunnan: Tectonic framework and tectonic evolution[J]. Journal of Jilin University: Earth Science Edition, 2011, 41(5): 1295~1303. http://www.cnki.com.cn/Article/CJFDTOTAL-CCDZ201105004.htm
[2] 许志琴, 李海兵, 唐哲民, 等.大型走滑断裂对青藏高原地体构架的改造[J].岩石学报, 2011, 27(11):3157~3170. http://www.cnki.com.cn/Article/CJFDTOTAL-YSXB201111001.htm
XU Zhi-qin. LI Hai-bing, TANG Zhe-min, et al. The transformation of the terrain structures of the Tibet Plateau through large-scale strike-slib faults[J]. Acta Petrologica Sinica, 2011, 27(11): 3157~3170. http://www.cnki.com.cn/Article/CJFDTOTAL-YSXB201111001.htm
[3] 张建国. 中越红河断裂带活动性研究[D]. 合肥: 中国科学技术大学, 2009: 1~3.
http://cdmd.cnki.com.cn/Article/CDMD-10358-2010042982.htm ZHANG Jian-guo. Research on the activity of Red River Fault in China and Vietnam[D]. Hefei: University of Science and Technology of China, 2009: 1~3.
[4] 王治华, 阎家盼, 郭晓东, 等.哀牢山构造带金矿床类型及成矿规律[J].黄金, 2011, 3(4):7~13 http://www.cnki.com.cn/Article/CJFDTOTAL-HJZZ201104004.htm
WANG Zhi-hua, YAN Jia-pan, GUO Xiao-dong, et al. Types and metallogenic regularity of gold deposits in Ailaoshan structural belt[J]. Gold, 2011, 32(4): 7~13. http://www.cnki.com.cn/Article/CJFDTOTAL-HJZZ201104004.htm
[5] 阚荣举, 张四昌, 晏凤桐, 等.我国西南地区现代构造应力场与现代构造活动特征的探讨[J].地球物理学报, 1997, 20(2):96~109. http://www.cnki.com.cn/Article/CJFDTOTAL-DQWX197702001.htm
KAN Rong-ju, ZHANG Si-chang, YAN Feng-tong, et al. Present tectonic stress field and its relation to the characteristics of recent tectonic activity Southwestern China[J]. Acta Geophysica Stnica, 1997, 20(2): 96~109. http://www.cnki.com.cn/Article/CJFDTOTAL-DQWX197702001.htm
[6] 谢富仁, 苏刚, 崔效锋, 等.滇西南地区现代构造应力场分析[J].地震学报, 2001, 23(1):17~23. http://www.cnki.com.cn/Article/CJFDTOTAL-DZXB200101002.htm
XIE Fu-ren, SU Gang, CUI Xiao-feng, et al. Modern tectonic stress field in southwestern Yunnan, China[J]. Acta Seismologica Sinica, 2001, 23(1): 17~23. http://www.cnki.com.cn/Article/CJFDTOTAL-DZXB200101002.htm
[7] 钱晓东, 秦嘉政, 刘丽芳.云南地区现代构造应力场研究[J].地震地质, 2011, 33(1):91~106. http://www.cnki.com.cn/Article/CJFDTOTAL-DZDZ201101011.htm
QIAN Xiao-dong, QIN Jia-zheng, LIU Li-fang. Study on recent tectonic stress field in Yunnan region[J]. Seismology and geology, 2011, 33(1): 91~106. http://www.cnki.com.cn/Article/CJFDTOTAL-DZDZ201101011.htm
[8] 王冬斌, 唐渊, 廖世勇, 等.滇西哀牢山变质岩系锆石U-Pb定年及其地质意义[J].岩石学报, 2013, 29(4):1261~1278. http://www.cnki.com.cn/Article/CJFDTOTAL-YSXB201304013.htm
WANG Dong-bin, TANG Yuan, LIAO Shi-yong, et al. Zircon U-Pb dating and its geological implications of the metamorphic of the metamorphic rock series in Ailaoshan Ranges, western Yunnan[J]. Acta Petrologica Sinica, 2013, 29(4): 1261~1278. http://www.cnki.com.cn/Article/CJFDTOTAL-YSXB201304013.htm
[9] 何希虎, 周瑞琦, 张双林, 等.红河断裂带地震地质特征[J].云南地质, 1983, 2(2):89~101. http://www.cnki.com.cn/Article/CJFDTOTAL-YNZD198302000.htm
HE Xi-hu, ZHOU Rui-qi, ZHANG Shuang-lin, et al. Geological and earthquake features of Red River fault zone[J]. Yunnan Geology, 1983, 2(2): 89~101. http://www.cnki.com.cn/Article/CJFDTOTAL-YNZD198302000.htm
[10] 云南省地质矿产局.云南省区域地质志[M].北京:地质出版社, 1990:1~658.
Bureau of Geology and Mineral Resource of Yunnan Province. Regional Geology of Yunnan Province[M]. Beijing: Geological Publishing House, 1990: 1~658.
[11] 张进江, 钟大赉, 桑海清, 等.哀牢山—红河断裂带古新世以来的多期活动的构造和年代学证据[J].地质科学, 2006, 41(2):291~310. http://kns.cnki.net/KCMS/detail/detail.aspx?filename=dzkx200602011&dbname=CJFD&dbcode=CJFQ
ZHANG Jin-jiang, ZHONG Da-lai, SANG Hai-qing, et al. Structural and geochronological evidence for multiple episodes of deformation since Paleocene along the Ailaoshan-Red River shear zone, southeastern Asia[J]. Chinese Journal of Geology, 2006, 41(2): 291~310. http://kns.cnki.net/KCMS/detail/detail.aspx?filename=dzkx200602011&dbname=CJFD&dbcode=CJFQ
[12] 曹淑云, 刘俊来, Bernd LEISS, 等.哀牢山—红河剪切带左行走滑作用起始时间约束:点苍山高温糜棱岩的显微构造与热年代学证据[J].地质学报, 2009, 83(10):1388~1400. doi: 10.3321/j.issn:0001-5717.2009.10.003
CAO Shuyun, LIU Junlaiz, Bernd LEISS, et al. Timing of initiation of left-lateral slip along the Ailaoshan-Red River shear zone: Microstructural, texture and thermochronological evidence from high temperature mylonites in Diancangshan, SW China[J]. Acta Geologica Sinica, 2009, 83(10): 1388~1400. doi: 10.3321/j.issn:0001-5717.2009.10.003
[13] 翟明国.中国滇西南造山带变质岩的Sm-Nd和Rb-Sr同位素年代学[J].岩石学报, 1990, (4):1~11. http://www.cnki.com.cn/Article/CJFDTOTAL-YSXB199004000.htm
ZHAI Ming-guo. Sm-Nd and Rb-Sr geochronology of metamorphic rocks from SW Yunnan orogenic zones, China[J]. Acta Petrologica Sinica, 1990, (4): 1~11. http://www.cnki.com.cn/Article/CJFDTOTAL-YSXB199004000.htm
[14] 李宝龙, 季建清, 付孝悦, 等.滇西点苍山—哀牢山变质岩系锆石SHRIMP定年及其地质意义[J].岩石学报, 2008, 24(10):2322~2330. http://www.cnki.com.cn/Article/CJFDTOTAL-YSXB200810013.htm
LI Bao-long, JI Jian-qing, FU Xiao-yue, et al. Zircon SHRIMP dating and its geological implications of the metamorphic rocks in Ailaoshan-Diancangshan Mountain Ranges, west Yunnan[J]. Acta Petrologica Sinica, 2008, 24(10): 2322~2330. http://www.cnki.com.cn/Article/CJFDTOTAL-YSXB200810013.htm
[15] 戚学祥, 朱路华, 李化启, 等.青藏高原东缘哀牢山—金沙江构造带糜棱状花岗岩的LA-ICP-MS U-Pb定年及其构造意义[J].地质学报, 2010, 84(3):357~369. http://www.cnki.com.cn/Article/CJFDTOTAL-DZXE201003006.htm
QI Xue-xiang, ZHU Lu-hua, LI Hua-qi, et al. Zircon LA-ICP-MS U-Pb dating for mylonitized granite from the Ailaoshan-Jinshajiang tectonic zone in the eastern Qinghai-Tibet Plateau and its tectonic significance[J]. Acta Geologica Sinica, 2010, 84(3): 357~369. http://www.cnki.com.cn/Article/CJFDTOTAL-DZXE201003006.htm
[16] 万天丰.构造应力场研究的新进展[J].地学前缘, 1995, 2(1/2):226~235. http://www.cnki.com.cn/Article/CJFDTOTAL-DXQY502.019.htm
WAN Tian-feng.The progress of researches on tectonic stress field [J]. Earth Science Frontiers, 1995, 2(1/2): 226~235. http://www.cnki.com.cn/Article/CJFDTOTAL-DXQY502.019.htm
[17] 刘迅.地质力学在矿田构造研究中的应用与进展[J].地质力学学报, 1996, 2(1):25~33. http://journal.geomech.ac.cn/ch/reader/view_abstract.aspx?flag=1&file_no=19960104&journal_id=dzlxxb
LIU Xun. Advance of application of geomechanics to the research of ore-field structures [J]. Journal of Geomechanics, 1996, 2(1): 25~33. http://journal.geomech.ac.cn/ch/reader/view_abstract.aspx?flag=1&file_no=19960104&journal_id=dzlxxb
[18] 万天丰.古构造应力场[M].北京:地质出版社, 1988:1~160.
WAN Tian-feng. Palaeotectonic stress filed[M]. Beijing: Geological Publishing House, 1988: 1~160.
[19] 胡玲, 刘俊来, 纪沫, 等.变形显微构造识别手册[M].北京:地质出版社, 2009:59~60.
HU Ling, LIU Jun-lai, JI Mo, et al. The manual of identification of deformational microscopic structures[M]. Beijing: Geological Publish House, 2009: 59~60.
[20] 陈正乐, 杨农, 王平安, 等.江西临川地区相山铀矿田构造应力场分析[J].地质通报, 2011, 30(4):514~531. http://www.cnki.com.cn/Article/CJFDTOTAL-ZQYD201104009.htm
CHEN Zheng-le, YANG Nong, WANG Ping-an, et al. Analysis of the tectonic stress field in the Xiangshan uranium ore field, Linchuan area, Jiangxi, China[J]. Geological Bulletin of China, 2011, 30(4): 514~531. http://www.cnki.com.cn/Article/CJFDTOTAL-ZQYD201104009.htm
[21] 邓宾, 刘树根, 杨锁, 等.林滩场构造多期节理构造特征及其意义[J].矿物岩石, 2009, 29(3):83~90. http://www.cnki.com.cn/Article/CJFDTOTAL-KWYS200903012.htm
DENG Bin, LIU Shu-gen, YANG Suo, et al. Structural characteristics of joins and its implication in the Linchang anticline[J]. Journal of Mineralogy and Petrology, 2009, 29(3): 83~90. http://www.cnki.com.cn/Article/CJFDTOTAL-KWYS200903012.htm
[22] 张加桂.从深部流动挤压格局分析西部的区域地壳稳定性[J].成都理工大学学报, 2001, 28(增刊):195~199. http://d.wanfangdata.com.cn/Periodical/cdlgxyxb2001z1042
ZHANG Jia-gui. Analysis of regional crustal stability from the framework of deep flow and thrust[J]. Journal of Chengdu University of Technology, 2001, 28(Supp.): 195~199. http://d.wanfangdata.com.cn/Periodical/cdlgxyxb2001z1042
-
下载:
图(8)
计量
- 文章访问数: 331
- PDF下载数: 5
- 施引文献: 0