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A study of the distribution characteristics of basin tectonic units based on gravity data in Madagascar and its adjacent basins |
Xue-Fa WANG1,2,3( ), Wan-Yin WANG1,2,3( ), Jie MA1,2,3, Min YANG1,2,3,4, Jian-She LIANG5, Chun-Guang QIU5, Ding-Ding WANG1,2,3, Xiao-Lin JI1,2,3, Jin-Lan LIU1,2,3 |
1. Insititute of Gravity and Magnetic Technology,Chang’an University,Xi’an 710054,China 2. College of Geology Engineering and Geomatics,Chang’an University,Xi’an 710054,China 3. Key Laboratory of Western China’s Mineral Resources and Geological Engineering,Ministry of Education,Chang’an University,Xi’an 710054,China 4. Department of Earth Sciences,Memorial University of Newfoundland,St.Johns’,A1B3X5,Canada 5. Cnooc Research Institute Limited,Beijing 100027,China |
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Abstract With offering the increasing opening exploration of oil and gas resources to the oversea exploration companies in Africa which remains in an early exploration stage, a good opportunity is provided for the companies in China. In this study, the gravity data of this research area were collected in order to study the tectonic characteristics of Malagasy Island, which has insufficient oil and gas geological data but abundant mineral resources. The faults and the boundaries of this basin were identified according to the response of the gravity anomaly to the sediments by the separation method of the minimum curvature, the vertical derivative of the normalized total horizontal derivative (NVDR-THDR) and the inversion of the depth of the curvature attribute, with Bouguer gravity anomaly. The geological and geophysical characteristics of the main faults were analyzed, and the distribution characteristics of faults and basins were determined, which were based on the geological and geophysical data. According to this research, there are 9 primary faults and 11 secondary faults inferred in this study area trending NNE, NE and nearly NS. The tectonics of Tamatave Basin, Morondava Basin and Majunga Basin were re-divided into 7 depressions and 3 uplifts combined with the distribution of faults from this study and previous studies, which are shown as a zonal distribution like "two depressions with one uplift". This research can provide geophysical information for exploration of oil, gas and mineral resources in Madagascar and its adjacent regions.
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Received: 18 February 2020
Published: 28 August 2020
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Corresponding Authors:
Wan-Yin WANG
E-mail: wxf20129@163.com;wwy7902@chd.rdu.cn
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14] ">
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Geological map of study area[14]
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1,2,3] ">
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Distribution map of study area fault and basin[1,2,3]
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Topography map of Madagascar
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Satellite altimetry gravity anomaly map of Madagascar
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Bouguer gravity anomaly map of Madagascar
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The plane location distribution of faults (a) and their apparent depth (b) in the Madagascar and its adjacent area
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The rose diagram of faults’strikes (a)and histogram of frequency distribution of faults’length(b) in the Madagascar
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Determined faults and the results of previous studies
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Faults and NVDR-THDR of Bouguer gravity anomaly
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Faults and Bouguer gravity anomaly
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编号 | 走向 | 位置 | 性质 | 长度/km | 备注 | F1-1 | NNE | 东部洋壳边界 | 扩张 | 1588 | 3 | F1-2 | NNE | 东部陆架—陆坡转换带 | 扩张 | 1596 | 3 | F1-3 | NEE | 南部洋壳边界 | 扩张 | 618 | 1 | F1-4 | NWW-NEE | 马达加斯加岛西部 | 扩张 | 1129 | 2 | F1-5 | NE | 马达加斯加岛北部 | 扩张 | 594 | 1 | F1-6 | 近EW | 北部洋壳边界 | 扩张 | 556 | 1 | F1-7 | NEE | 北部洋壳边界 | 扩张 | 803 | 1 | F1-8 | 近SN | 西部洋壳边界 | 走滑 | 2445 | 2 | F1-9 | 近SN | 西部陆架—陆坡转换带 | 走滑 | 2023 | 2 |
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The statistical table of attributes of first-class fault
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Determined boundaries of basinand the results of previous studies
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Sediments of regional gravity anomaly map in Madagascar
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Sediments of residual gravity anomaly map in Madagascar
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Thickness of sedimentary mapof Madagascar
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Tectonic division map of Madagascar
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