Identification and new discovery of Qiansxuilan fault belt in Gaudeanmus area, Namibia based on the multi-source remote sensing data
-
摘要: 遥感影像因其可直观显示地质构造形迹的物理特征及地表形态,弥补野外点线观测的局限性,在成矿环境识别及资源评价领域受到众多地学工作者的青睐。以纳米比亚欢乐谷白岗岩型铀成矿区为研究区,基于ETM+、Radarsat-2多源遥感数据,通过开展彩色合成、纹理信息提取、光学和雷达信息融合等图像信息增强,从地层、岩体、构造、地形、水系、植被等方面构建了千岁兰断裂带遥感解译标志,如岩体、岩层被切割、错开或呈穹窿状,地貌为破碎的山体垭口形态或地形切割强烈破碎的深沟,发育硅化、高岭土化、钾化、方解石化、绿泥石化蚀变现象等。基于构建的遥感解译标志和断裂识别方法,识别出了区内部分出露、部分隐伏、规模最大且最重要的千岁兰控矿断裂,创新性提出了千岁兰断裂在区内并非为1组断裂,而是由北部、中部、南部3组断裂组成的断裂带。结合野外出露断裂判别特征和控矿作用分析,验证了千岁兰断裂带的真实存在,且正是该断裂带控制着区内含铀白岗岩和铀矿化的产出。Abstract: Because the images could display the physical characteristics and their surface morphology of geological structures intuitively and make up for the limitations of field investigation, remote sensing technology is favored by many geoscientists in the field of mineralization environment identification and resource evaluation. The paper took the leucogranite-type uranium metallogenic area in Gaudeanmus, Namibia as the research area, carried out the information enhancement of images such as color composition, texture information extraction, optical and radar image fusion, and constructed the marks for fault identification from stratum, leucogranite bodies, structure, geomorphology, water system, vegetation and so on, based on the multi-source remote sensing data of ETM+ and Radarsat-2.Leucogranite bodies and layers were cut or folded to form a vault.The landform appeared as a tectonic fracture, silicification, kaolinization, potassic alteration, calcitization, chloritization and were developed. Furthermore, the paper identified the partly outcropping and partly buried fault named Qiansuilan that was the largest and most important ore-controlled fault in the region, based on the fault identification marks and method. Furthermore, it was proposed innovatively that the Qiansuilan fault was not a group of faults in the area, but a fault zone consisting of three groups of faults named the northern, central and southern faults zone. Combined with the fault identification feature exposed in the field and ore-controlling analysis, the Qiansuilan fault existed truly and it controlled the occurrence of leucogranite rich in uranium and uranium mineralization in the area.
-
Key words:
- multi-source remote sensing /
- Namibia /
- Gaudeanmus /
- Qiansuilan fault /
- new discovery
-
图 1 欢乐谷地区铀矿地质简图(据文献[8]修改)
Figure 1. Uranium geological diagram of Gaudeanmus area, Namibia
-
[1] 顾大钊, 范洪海, 舒良树, 等.纳米比亚欢乐谷地区构造演化对铀成矿的制约[J].地质论评, 2016, 62(1):83-94. http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=dzlp201601008 [2] 陈金勇, 范洪海, 王生云, 等.纳米比亚欢乐谷地区白岗岩型铀矿成矿物质来源分析[J].地质学报, 2016, 90(2):219-230. http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=dizhixb201602002 [3] 赵希刚, 朱西养, 杨永记, 等.纳米比亚达马拉造山带白岗岩型铀矿成矿规律及找矿思路[J].铀矿地质, 2015, 31(4):445-453. http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=ykdz201504005 [4] Corvino A F, Pretorius L E.Uraniferous leucogranites south of Ida Dome, central Damara Belt, Namibia:Morphology, distribution and mineralization[J].Journal of African Earth Sciences, 2013, 80(6):60-73. http://www.sciencedirect.com/science/article/pii/S1464343X13000046 [5] Kinnaird J A, Nex P A M.A review of geological controls on uranium mineralization in sheeted leucogranites within the Damara Orogen, Namibia[J].Applied Earth Science, 2007, 116(2):68-85. doi: 10.1179/174327507X167091 [6] Nex P A M, Kinnaird J A, Oliver G J H.Petrology, geochemistry and uranium mineralization of post collisional magmatism around Goanikontes, southern Central Zone, Namibia[J].Journal of African Earth Sciences, 2001, 33(1):481-502. http://www.sciencedirect.com/science/article/pii/S0899536201000963 [7] Basson I J, Greenway G.The Rössing uranium deposit:A product of late-kinematic location of uraniferous granites in the Central Zone of the Damara Orogen, Namibia[J].Journal of African Earth Sciences, 2004, 38(12):413-435. http://www.sciencedirect.com/science/article/pii/S0899536204000545 [8] 陈金勇, 范洪海, 陈东欢, 等.纳米比亚欢乐谷地区白岗岩型铀矿矿物特征研究[J].地质论评, 2013, 59(5):962-970. http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=dzlp201305018 [9] 徐俊龙, 温兴平, 张浩楠, 等.遥感线性构造中心对称度的尺度效应研究[J].地质科技情报, 2019, 38(3):290-300. http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=dzkjqb201903032 [10] 张毅, 李细光, 张雄.融合多元遥感信息的新右江次级活动断裂解译[J].武汉大学学报:信息科学版, 2015, 40(8):1023-1030. http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=whchkjdxxb201508006 [11] 何国金, 李克鲁.星载合成孔径雷达遥感及多卫星遥感数据融合方法[J].地质科技情报, 1997, 16(增刊1):29-35. http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=QK199700065702 [12] 代晶晶.PALSAR及RADARSAT2全极化雷达数据在地质构造应用中的研究[J].地质与勘探, 2011, 47(4):719-724. http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=dzykt201104022 [13] 张亮, 那晓东, 刘知, 等.基于国产GF-2卫星影像的遥感地质解译:以阿吾拉勒地区为例[J].地质科技情报, 2018, 37(2):233-240. http://www.cqvip.com/QK/93477A/20182/674988999.html [14] Nance R D, Murphy J B, Santosh M.The supercontinent cycle:A retrospective essay[J].Gondwana Research, 2014, 25(9):4-29. http://www.sciencedirect.com/science/article/pii/S1342937X13000506 [15] Anderson H, Nash C.Integrated lithostructural mapping of the Rössing area, Namibia using high resolution aeromagnetic, radiometric Landsat data and aerial photographs[J].Exploration Geophysics, 1997, 28(3):185-191. http://www.publish.csiro.au/eg/EG997185 [16] Poli L C, Oliver G J H.Constrictional deformation in the Central Zone of the Damara Orogen, Namibia[J].Journal of African Earth Science, 2001, 33(5):303-312. http://www.sciencedirect.com/science/article/pii/S0899536201800658 [17] Longridge L, Gibson R L, Kinnaird J A, et al.Timing of deformation and granite emplacement in the central zone of the Damara Orogen, Namibia[R].Johannesburg: School of Geosciences, University of the Witwatersrand, 2008(Unpublished report). [18] Berning J, Cooke R, Heimstra S, et al.The Rössing uranium deposit, South West Africa[J].Economic Geology, 1976, 71(24):351-368. [19] 田青林, 潘蔚, 李瀚波, 等.基于多源遥感数据的蚀变信息提取对比研究[J].地质科技情报, 2018, 37(6):218-225. http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=dzkjqb201806027 [20] Shelat Y, Leblon B.Radarsat-2 polarimetric SAR imagery:An aid for assessing the uranium potential of the paleo Proterozoic Thelon Basin, Nunavut[J].Geological Survey of Canada, 2010(4):1-4. http://www.researchgate.net/publication/266222155_RADARSAT-2_Polarimetric_SAR_Imagery_An_Aid_for_Assessing_the_Uranium_Potential_of_the_Paleoproterozoic_Thelon_Basin_Nunavut [21] Paradella W R, Bignelli P A, Veneziani P, et al.Airborne and spaceborne Synthetic Aperture Radar(SAR)integration with Landsat TM and gamma ray spectrometry for geological mapping in a tropical rainforest environment, the Carajas Mineral Province, Brazil[J].International Journal of Remote Sensing, 1997, 18(7):1483-1501. doi: 10.1080/014311697218232 [22] Oliver G J H, Kinnaird J A.The Rossing SJ Dome, Central Zone, Damara Belt, Namibia:An example of mid-crustalex-tensional ramping[J].Communications of the Geological Survey of Namibia, 1996, 11(7):53-64. http://www.researchgate.net/publication/292231296_The_Rossing-SJ_Dome_Central_Zone_Damara_Belt_Namibia_an_example_of_mid-crustal_extensional_ramping [23] Miller R.The geology of Namibia[M].Windhoek:Geological Survey of Namibia Special Publication, 2008.