APPLICATION OF REMOTE SENSING TECHNIQUE IN THE MAPPING OF CENOZOIC GEOLOGY OF THE EAST KUNLUN MOUNTAINS
-
摘要:
利用不同地质体在同一波段或相同地质体在不同波段具有不同色调的变化规律，对东昆仑东温泉盆地的ETM图像进行了详细地质解译，建立了新生代地层和新构造的解译标志。解译结果表明，在遥感图像上可以准确勾绘新生代地层的界线和确定新生代断裂位置。通过野外地质验证将新生代地层划分为10个填图单位，新生代断裂主要有近东西向的左旋走滑断裂和近北西西向的逆冲推覆构造。遥感地质解译和野外验证结果对比表明，多光谱遥感影像在新生代地质填图中可以发挥重要作用。
Abstract:According to the color variations of different geological bodies in the same wave band or the same geological body in different wave bands, a close geological interpretation has been made for the ETM images from the East Wenquan Basin of the east Kunlun Mountains, resulting in the establishment of interpretation makers for the Cenozoic strata and new structures. The interpretation allows us to accurately define the Cenozoic strata boundaries and Cenozoic fault locations on the ETM images. The Cenozoic strata in the mapping area can be divided into 10 mapping units based on the field survey. The Cenozoic faults include nearly NW left-lateral strike-slip faults and nearly NWW thrust nappe structures. It is believed that multispectral remote sensing image can play an important role in Cenozoic geological mapping.
-
Key words:
- remote sensing /
- Cenozoic strata /
- Cenozoic structure /
- East Wenquan Basin /
- East Kunlun Mountains
-
-
表 1 东温泉盆地新生代地层遥感解译标志
Table 1. Remote sensing interpretation of Cenozoic strata in East Wenquan Basin
下载: 导出CSV
-
[1] 毕思文.全球变化与地球系统科学统一研究的最佳天然实验室———青藏高原[J].系统工程理论与实践, 1997, (5) : 72 ~ 77. https://core.ac.uk/display/155323393
BI Si-wen. A best laboratory of the universal research for the earth's global change and earth system science: The QinghaiTibet Plateau[J]. Systems Engineering Theory & Practice, 1997, (5) : 72 ~ 77. https://core.ac.uk/display/155323393
[2] 郑度, 姚檀栋.青藏高原隆升及其环境效应[J].地球科学进展, 2006, 21 (5) : 451 ~ 458. http://d.old.wanfangdata.com.cn/Periodical/dqkxjz200605002
ZHENG Du, YAO Tan-dong. Uplifting of Tibetan Plateau with its environmental effects[J]. Advances in Earth Science, 2006, 21 (5) : 451 ~ 458. http://d.old.wanfangdata.com.cn/Periodical/dqkxjz200605002
[3] 宋春晖, 方小敏, 李吉均, 等.青藏高原东北部贵德盆地上新世沉积环境分析及其意义[J].第四纪研究, 2003, 23 (1) : 93 ~ 102. http://d.old.wanfangdata.com.cn/Periodical/dsjyj200301011
SONG Chun-hui, FANG Xiao-min, LI Ji-jun, et al. Pliocene sedimentary environment of the northeast margin of the Qinghai-Tibetan Plateau and its significance[J]. Quaternary Science, 2003, 23 (1) : 93 ~ 102. http://d.old.wanfangdata.com.cn/Periodical/dsjyj200301011
[4] 张振, 宋春晖, 张平, 等.青藏高原昆仑山垭口盆地晚上新世以来沉积物磁化率与气候变化[J].资源调查与环境, 2007, 28 (3) : 205 ~ 213. http://d.old.wanfangdata.com.cn/Periodical/hsdzykc200703008
ZHANG Zhen, SONG Chun-hui, ZHANG Ping, et al. Magnetic susceptibilitsy of lacustrine sediments and climatic change in Kunlun Mountains Pass Basin since the Late Pliocene[J]. Resources Survey & Environment, 2007, 28 (3): 205 ~ 213. http://d.old.wanfangdata.com.cn/Periodical/hsdzykc200703008
[5] 吴中海, 赵希涛, 吴珍汉, 等.西藏纳木错地区约120 ka BP以来的古植被、古气候与湖面变化[J].地质学报, 2004, 78 (2) : 242 ~ 252. http://d.old.wanfangdata.com.cn/Periodical/dizhixb200402014
WU Zhong-hai, ZHAO Xi-tao, WU Zhen-han, et al. Palaeovegetation, palaeeclimate and lake-level change since 120 ka BP in Nam Co, central Xizang[J]. Acta Geologica Sinica, 2004, 78 (2) : 242 ~ 252. http://d.old.wanfangdata.com.cn/Periodical/dizhixb200402014
[6] 郑绵平, 袁鹤然, 赵希涛, 等.青藏高原第四纪泛湖期与古气候[J].地质学报, 2006, 80 (2) : 169 ~ 180. http://d.old.wanfangdata.com.cn/Periodical/dizhixb200602001
ZHENG Mian-ping, YUAN He-ran, ZHAO Xi-tao, et al. The Quaternary pan-lake (overflow) period and paleoclimate on the Qinghai-Tibet Plateau[J]. Acta Geologica Sinica, 2006, 80 (2) : 169 ~ 180. http://d.old.wanfangdata.com.cn/Periodical/dizhixb200602001
[7] 赵希涛, 郑绵平, 李道明.青海格尔木三岔河组年龄测定与昆仑古湖发育[J].第四纪研究, 2009, 29 (1): 89 ~ 97. http://d.old.wanfangdata.com.cn/Periodical/dsjyj200901010
ZHAO Xi-tao, ZHENG Mian-ping, LI Dao-ming. Dating of the Sanchahe Formation and development of Kunlun paleolake in Golmud City, Qinghai Province[J]. Quaternary Science, 2009, 29 (1) : 89 ~ 97. http://d.old.wanfangdata.com.cn/Periodical/dsjyj200901010
[8] 吴绍洪, 尹云鹤, 郑度, 等.青藏高原近30年气候变化趋势[J].地理学报, 2005, 60 (1) : 3 ~ 11. doi: 10.11821/xb200501001
WU Shao-hong, YIN Yun-he, ZHENG Du, et al. Climate changes in the Tibetan Plateau during the last three decades [J]. Acta Geographica Sinica, 2005, 60 (1) : 3 ~ 11. doi: 10.11821/xb200501001
[9] 郑度, 林振耀, 张雪芹.青藏高原与全球环境变化研究进展[J].地学前缘, 2002, 9 (1) : 95 ~ 102. http://d.old.wanfangdata.com.cn/Periodical/dxqy200201012
ZHENG Du, LIN Zhen-yao, ZHANG Xue-qin. Progress in studies of Tibetan Plateau and global environmental change [J]. Earth Science Frontiers, 2002, 9 (1) : 95 ~ 102. http://d.old.wanfangdata.com.cn/Periodical/dxqy200201012
[10] 李建国, 周勇.西藏札达盆地晚上新世古植被型分析[J].古地理学报, 2002, 4 (1) : 52 ~ 58. doi: 10.7605/gdlxb.2002.01.006
LI Jian-guo, ZHOU Yong. Palaeovegetation type analysis of the Late Pliocene in Zanda Basin of Tibet[J]. Journal of Palaeogeography, 2002, 4 (1) : 52 ~ 58. doi: 10.7605/gdlxb.2002.01.006
[11] 倪晋宇, 胡道功, 周春景.东昆仑造山带纳赤台群形成的大地构造环境探讨[J].地质力学学报, 2010, 16 (1) : 11 ~ 20. http://journal.geomech.ac.cn/ch/reader/view_abstract.aspx?flag=1&file_no=20100102&journal_id=dzlxxb
NI Jin-yu, HU Dao-gong, ZHOU Chun-jing. Discussion on tectonic environment of Naij Tal Group, East Kunlun orogenic belt[J]. Journal of Geomechanics, 2010, 16 (1) : 11 ~ 20. http://journal.geomech.ac.cn/ch/reader/view_abstract.aspx?flag=1&file_no=20100102&journal_id=dzlxxb
[12] 周春景, 胡道功, Barosh P J, 等.东昆仑三道湾流纹英安斑岩锆石U-Pb年龄及其地质意义[J].地质力学学报, 2010, 16 (1) : 28 ~ 35. http://journal.geomech.ac.cn/ch/reader/view_abstract.aspx?flag=1&file_no=20100104&journal_id=dzlxxb
ZHOU Chun-jing, HU Dao-gong, Barosh P J, et al. Zircon U-Pb dating of the rhyolite-dcite porphyry in the Sandaowan of east Kunlun MTS and its geological significance[J]. Journal of Geomechanics, 2010, 16 (1) : 28 ~ 35. http://journal.geomech.ac.cn/ch/reader/view_abstract.aspx?flag=1&file_no=20100104&journal_id=dzlxxb
[13] 陆露, 胡道功, 张永清, 等.昆中断裂带同构造花岗斑岩锆石U-Pb年龄及其构造意义[J].地质力学学报, 2010, 16 (1) : 36 ~ 43. http://journal.geomech.ac.cn/ch/reader/view_abstract.aspx?flag=1&file_no=20100105&journal_id=dzlxxb
LU Lu, HU Dao-gong, ZHANG Yong-qing, et al. Ziron U-Pb age for syntectoin granitic porphyry and its teceonic significance in the middle Kunlun fallt belt[J]. Journal of Geomechanics, 2010, 16 (1) : 36 ~ 43. http://journal.geomech.ac.cn/ch/reader/view_abstract.aspx?flag=1&file_no=20100105&journal_id=dzlxxb
[14] 吴芳, 张绪教, 张永清, 等.东昆仑闹仓坚沟组流纹质凝灰岩锆石U-Pb年龄及其地质意义[J].地质力学学报, 2010, 16 (1) : 44 ~ 50. http://journal.geomech.ac.cn/ch/reader/view_abstract.aspx?flag=1&file_no=20100106&journal_id=dzlxxb
WU Fang, ZHANG Xu-jiao, ZHANG Yong-qing, et al. Zircon U-Pb ages for rhyolite tuff of the Naocangjiangou Formation in the east Kulun orogenic belt and their implication[J]. Journal of Geomechanics, 2010, 16 (1) : 44 ~ 50. http://journal.geomech.ac.cn/ch/reader/view_abstract.aspx?flag=1&file_no=20100106&journal_id=dzlxxb
[15] 张紫程, 张绪教, 高万里, 等.东昆仑左行韧性剪切带形成时代的锆石U-Pb年龄证据[J].地质力学学报, 2010, 16 (1) : 51 ~ 58. http://journal.geomech.ac.cn/ch/reader/view_abstract.aspx?flag=1&file_no=20100107&journal_id=dzlxxb
ZHANG Zi-cheng, ZhANG Xu-jiao, GAO Wan-li, et al. Evidence of zircon U-Pb ages for the formation time of the east Kunlun left-lateral ductile shear belt[J]. Journal of Geomechanics, 2010, 16 (1) : 51 ~ 58. http://journal.geomech.ac.cn/ch/reader/view_abstract.aspx?flag=1&file_no=20100107&journal_id=dzlxxb
[16] 张耀玲, 张绪教, 胡道功, 等.东昆仑造山带纳赤台群流纹岩SHRIMP锆石U-Pb年龄[J].地质力学学报, 2010, 16 (1) : 21 ~ 27, 50. http://journal.geomech.ac.cn/ch/reader/view_abstract.aspx?flag=1&file_no=20100103&journal_id=dzlxxb
ZHANG Yao-ling, ZHANG Xu-jiao, HU Dao-gong, et al. SHRIMP-based zircon U-Pb ages for rhyolite of the Naij Tal Group in the east Kulun orogenic belt[J]. Journal of Geomechanics, 2010, 16 (1) : 21 ~ 27, 50. http://journal.geomech.ac.cn/ch/reader/view_abstract.aspx?flag=1&file_no=20100103&journal_id=dzlxxb
[17] 高万里, 张绪教, 王志刚, 等.基于ASTER遥感图像的东昆仑造山带岩性信息提取研究[J].地质力学学报, 2010, 16 (1) : 59 ~ 69. http://journal.geomech.ac.cn/ch/reader/view_abstract.aspx?flag=1&file_no=20100108&journal_id=dzlxxb
GAO Wan-li, ZHANG Xu-jiao, WANG Zhi-gang, et al. ASTER remote sensing image-based lithologic information extraction of the east Kulun orogenic belt[J]. Journal of Geomechanics, 2010, 16 (1) : 59 ~ 69. http://journal.geomech.ac.cn/ch/reader/view_abstract.aspx?flag=1&file_no=20100108&journal_id=dzlxxb
[18] 张绪教, 李团结, 陆平, 等.卫星遥感在西藏安多幅1 : 25万区域第四纪地质调查中的应用[J].现代地质, 2008, 22 (1) : 107 ~ 115.
ZHANG Xu-jiao, LI Tuan-jie, LU Ping, et al. Application of satellite remote sensing to 1: 250 000 regional Quaternary investigation in Amdo sheet, Tibet[J]. Geoscience, 2008, 22 (1) : 107 ~ 115.
[19] 张玉明, 白朝军, 方怀宾. TM数据在西藏活动构造解译中的应用[J].国土资源遥感, 2002, 4 (54): 37 ~ 39. http://d.old.wanfangdata.com.cn/Periodical/gtzyyg200204008
ZHANG Yu-ming, BAI Chao-jun, FANG Huai-bin. The application of TM data to active tectonic zones in Tibet[J]. Remote Sensing for Land & Resources, 2002, 4 (54) : 37 ~ 39. http://d.old.wanfangdata.com.cn/Periodical/gtzyyg200204008
[20] 杨晓平.基于TM遥感图像的流域地貌研究[J].科技通报, 2003, 19 (2) : 150 ~ 153. http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=kjtb200302017
YANG Xiao-ping. Study on river basin landform based on TM remote sensing image[J ]. Bulletin of Science and Technology, 2003, 19 (2) : 150 ~ 153. http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=kjtb200302017
[21] 冯佐海, 梁金城, 张桂林, 等.平桂地区遥感线性构造的分形特征及其地质意义[J].地球学报, 2002, 23 (6) : 563 ~ 566. http://d.old.wanfangdata.com.cn/Periodical/dqxb200206014
FENG Zuo-hai, LIANG Jin-cheng, ZHANG Gui-lin, et al. Fractal characteristics of remote sensing lineations in Pinggui area and their geological significance[J]. Acta Geoscientia Sinica, 2002, 23 (6) : 563- 566. http://d.old.wanfangdata.com.cn/Periodical/dqxb200206014
[22] 崔志强, 刘登忠, 刘志强, 等.西藏措勤盆地新构造运动遥感研究[J].新疆地质, 2007, 25 (3) : 313 ~ 316. http://d.old.wanfangdata.com.cn/Periodical/xjdz200703018
CUI Zhi-qiang, LIU Deng-zhong, LIU Zhi-qiang, et al. The study of Neotectonic movement in Cuoqin Basin based on remote sensing technique[J]. Xinjiang Geology, 2007, 25 (3) : 313 ~ 316. http://d.old.wanfangdata.com.cn/Periodical/xjdz200703018
[23] 韩玲, 王润平.武都-文县地区遥感影像线性构造解译[J].地球科学与环境学报, 2008, 30 (4) : 434 ~ 437. http://d.old.wanfangdata.com.cn/Periodical/xagcxyxb200804019
HAN Ling, WANG Run-ping. Remote sensing image interpretation of linear tectonics in Wudu-Wenxian area[J]. Journal of Earth Sciences and Environment, 2008, 30 (4) : 434 ~ 437. http://d.old.wanfangdata.com.cn/Periodical/xagcxyxb200804019
[24] 施美凤, 李亚林, 于学政.西藏冈底斯地区水系格局与新构造活动关系的遥感研究[J].国土资源遥感, 2008, (3) : 69 ~ 73. doi: 10.6046/gtzyyg.2008.03.16
SHI Mei-feng, LI Ya-lin, YU Xue-zheng. A remote sensing study of the relationship between water system pattern and Neotectonic movement of Gangdise block in Tibet Plateau[J]. Remote Sensing for Land & Resources, 2008, (3) : 69 ~ 73. doi: 10.6046/gtzyyg.2008.03.16
[25] 吴珍汉, 胡道功, 吴中海, 等.青藏高原新生代构造演化与隆升过程[M].北京:地质出版社, 2009. 16 ~ 70.
WU Zhen-han, HU Dao-gong, WU Zhong-hai, et al. Cenozoic tectonic evolution and uplift process of the Tibetan Plateau [M]. Beijing: Geological Publishing House, 2009. 16 ~ 70.
[26] 胡道功, 叶培盛, 吴芳, 等.东昆仑断裂带西大滩段晚第四纪古地震历史[J].第四纪研究, 2008, 28 (2): 214 ~ 221. http://d.old.wanfangdata.com.cn/Periodical/dsjyj200802003
HU Dao-gong, YE Pei-sheng, WU Fang, et al. Late Quaternary paleoseismic history on the Xidatan segment of the East Kunlun fault zone in northern Tibet[J]. Quaternary Sciences, 2008, 28 (2) : 214 ~ 221. http://d.old.wanfangdata.com.cn/Periodical/dsjyj200802003
[27] 胡道功, 叶培盛, 吴珍汉, 等.东昆仑断裂带西大滩段全新世古地震研究[J].第四纪研究, 2006, 26 (6): 1012 ~ 1020. http://d.old.wanfangdata.com.cn/Periodical/dsjyj200606018
HU Dao-gong, YE Pei-sheng, WU Zhen-han, et al. Research on Holocene paleoearthquakes on the Xidatan segment of East Kunlun fault zone in northern Tibet[J]. Quaternary Sciences, 2006, 26 (6) : 1012 ~ 1020. http://d.old.wanfangdata.com.cn/Periodical/dsjyj200606018
-
图(3)
表(1)
计量
- 文章访问数: 474
- PDF下载数: 2
- 施引文献: 0