|
|
Gravity method application in tectonic characters and rock mass interpretation of Qilian Mountains |
LU Lichun1, JIANG Hong2, WU Ronggao1, ZHANG Pei3, ZHANG Chong4, LI Longfeng5 |
1. NO.2 Comprehensive Geophysical Prospecting Brigade, Shaanxi Geology and Mining Group Co. Ltd., Xi’an 710016, China; 2. Shananxi Hanzhong Geological Brigade, Geology and Mineral and Mining Group Co. Ltd., Hanzhong 723000, China; 3. The Second Crust Monitoring and Application Center, China Earthquake Administration, Xi’an 710054, China; 4. SinoProbe Center-China Deep Exploration Center, Chinese Academy of Geological Sciences, Beijing 100037,China; 5. Second Institute Geology and Mineral Resources, Gansu Bureau of Geology and MineralExploration and Development, Lanzhou 730022, China |
|
|
Abstract Based on geological, aeromagnetic and other data, and combined with measured physical properties of rock, the authors conducted a comprehensive research on Qilian Mountains (Zhangye and Gangcha areas) with the 1∶250 000 gravity data. The geological structure characteristics, geophysical characteristics, division of tectonic units and distribution of concealed and semi-concealed rock mass were studied. After many years’ gravity work in this area, the exploration area has reached nearly 30 000 km2. This paper has studied the characteristics of Bouguer gravity field based on gravity data and has divided the anomaly units. The geological tectonic units have been redivided and the major faults have been discussed. Concealed and semi-concealed rock mass have been identified and the spatial distributions have been speculated and interpreted. The results show that the partition and stratification of the crust density structure in Qilian Mountains are obvious, and that the partition characteristics of the Bouguer gravity anomaly field are basically the same with the partition characteristics of the geological structure. The combination of 2.5D gravity section inversion confirms the new speculations. The results will provide some reference for comprehensive geological and geophysical prospecting.
|
Received: 11 May 2017
|
|
|
|
|
[1] 张伯宏,刘天铭,祝意青.河西—祁连山重复重力测量资料的地震前兆信息研究[J].地震,1997,17(3):304-312. [2] 向鼎璞. 祁连山地质构造特征[J].地质科学,1982(4):364-370. [3] 郭原生,孙淑荣,代文昭,等.祁连山西段蛇绿岩型超基性岩特征及其地质意义[J].甘肃地质学报,1993,2(2):34-44,108. [4] 周良仁,秦克令.北祁连山超基性岩体接触变质特征及其地质意义[J].地质论评,1980,26(6):490-498. [5] 魏春海. 中国祁连山地质构造的基本特征[J].地质学报,1978,52(2):95-105. [6] 中国科学院地质研究所.祁连山地质志[M].北京:科学出版社,1963. [7] 冯益民. 祁连造山带研究概况——历史、现状及展望[J].地球科学进展,1997,12(4):307-314. [8] 向鼎璞. 祁连山主要地质特征[G]//青藏高原地质文集(17).北京:地质出版社,1985:61-79. [9] 冯益民,何世平.祁连山大地构造与造山作用[M].北京:地质出版社,1996. [10] 中国科学院地质研究所构造地质室.中国大地构造图[M].北京:地图出版社,1979. [11] 夏林圻,夏祖春,徐学义.北祁连山海相火山岩岩石成因[M].北京:地质出版社,1996. [12] 夏林圻,夏祖春,任有祥,等.祁连、秦岭山系海相火山岩[M].武汉:中国地质大学出版社,1991. [13] 吴荣高,路利春,崔丽艳,等.青海1∶25万刚察县幅、张掖市幅基础地质调查修测成果报告[R].西安:陕西省地质矿产勘查开发局第二综合物探大队,2015. [14] 黄瑞琦. 祁连山地质构造特征研究[J].西部资源,2016(5):9-10. [15] 计文化,杨博,姜寒冰,等.西北主要成矿带地质矿产调查工程进展[J].中国地质调查,2017,4(6):1-8. [16] 崔作舟,李秋生,吴朝东,等.格尔木—额济纳旗地学断面的地壳结构与深部构造[J].地球物理学报,1995,38(增刊2):15-28. [17] 彭礼贵,任有祥,李智佩,等.甘肃省白银厂铜多金属矿床成矿模式[M].北京:地质出版社,1995. [18] 邬介人,任秉琛,黄玉春,等.西北海相火山岩地区块状硫化物矿床[M].武汉:中国地质大学出版社,1994:232-234. [19] 李家斌,朱大友,屈念念,等.高精度重力方法在"大塘坡式"锰矿找矿中的应用[J].中国地质调查,2016,3(2):15-20. [20] 郭周平,赵辛敏,白赟.北祁连山银灿铜矿矿床地质特征及成因[J].中国地质调查,2015,2(3):54-58. [21] 张照伟,李文渊,高永宝.祁连—龙首山元古宙大火成岩省与金川型铜镍矿关系探讨[J].中国地质调查,2014,1(1):14-18. [22] 路利春,文博,程斌,等.成像技术在矿区重力勘探中的应用研究[J].地质与资源,2018,27(1):99-102,88. [23] 路利春,王鹏,周明霞,等.渭河盆地重力场与构造特征关系研究[J].大地测量与地球动力学,2017,37(增刊1):36-42. [24] 路利春,赵炳坤,周明霞,等.高精度重磁测量在渭河盆地氦气调查中的应用研究[J].陕西地质,2017,35(2):52-59. [25] ΓайнаHов А Γ.陈邦彦,译.地球重力场和大地构造[J].海洋地质译丛,1992(3):39-46. [26] 祝恒宾,周文虎,武立高.青藏高原重力场特征及其在大地构造上的含义[G]//中国科学院地球物理研究所论文摘要集(1985).北京:中国科学院地球物理研究所,1989:2. [27] 杨宗仁. 中国区域重力场的大地构造意义[J].大地构造与成矿学,1988,12(2):155-164. [28] 张凤旭,张兴洲,张凤琴,等.中国东北地区重力场研究——利用改进的三方向小子域滤波划分主构造线及大地构造单元[J].地球物理学报,2010,53(6):1475-1485. [29] 程顺有. 中央造山系及其邻区岩石圈三维结构与动力学意义[D].西安:西北大学,2006. [30] 闫雅芬,王光杰,张中杰.华南大陆重力场特征及其大地构造意义[C]//中国地球物理学会年刊2002——中国地球物理学会第十八届年会论文集.北京:中国地球物理学会,2002:1. [31] 夏林圻,李向民,余吉远,等.祁连山新元古代中—晚期至早古生代火山作用与构造演化[J].中国地质,2016,43(4):1087-1138. [32] 李冰. 祁连山典型地区新生代构造地貌演化过程研究[D].北京:中国地质大学(北京),2016. [33] 戚帮申. 祁连山新生代构造地貌演化特征[D].北京:中国地质大学(北京),2014. [34] 李世金. 祁连造山带地球动力学演化与内生金属矿产成矿作用研究[D].长春:吉林大学,2011. |
[1] |
ZHANG Zhaoqi, WANG Quan, WEI Yansheng, LIU Chengru, YANG Wubao, DUAN Chunsen, YANG Yaohua. Main achievements in supplemental regional geological survey of 1∶250 000 Datong Sheet[J]. , 2017, 4(4): 50-59. |
[2] |
WANG Weiping, WANG Defa, WU Chengping. Aeromagnetic feature and structure units division in Xilinhot-Xiwuqi aera[J]. , 2017, 4(1): 35-38. |
|
|
|
|