| 扬子地区盆褶山系深部结构的动力学探究 |
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| 引用本文： | 范小林,陆国新.扬子地区盆褶山系深部结构的动力学探究[J].石油实验地质,1993,15(4):335-342. |
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| 作者姓名： | 范小林 陆国新 |
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| 作者单位： | 地质矿产部石油地质中心实验室 无锡 214151 |
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| 基金项目： | 地矿部75-054-02-01-01-05专题“扬子地区区域地球物理场的综合地质解释和深部地质组成”部分成果 |
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| 摘 要： | 本文根据地震测深、大地电磁测探、大地热流测量资料整理汇编成有关图表,结合区域地质与岩石学研究成果进行对比,综合分析扬子地区岩石圈物性特征(波速、密度、电阻率、大地热流值)所反映的结构与构造特征,探索该区自中生代以来,在新全球构造体制下的盆褶山系形成、演化的动力学条件。
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| 关 键 词： | 扬子地区 盆地与造山带 深部结构 地动力学条件 |
| 收稿时间： | 1991-11-11 |
ON THE DYNAMIC RESEARCH OF THE DEEP-SEATED STRUCTURE FOR THE BASIN-FOLD-MOUNTAIN SYSTEM IN YANGTZE AREA |
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| Affiliation: | Central Laboratory of Petroleum Geology, MGMR |
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| Abstract: | According to the data of seismic sounding, magnetotelluric sounding and the geother-mal flow measurement, a variety of planimetric maps and diagrams have been charted. Compared with the results of the regional geology and lithology research, the characteristic of the physical properties of the lithosphere (velocity, density, resistivity, heat flow etc.) in Yangtze area have been analyzed comprehensively. This paper has also researched the dynamical condition of the basin-fold-mountain system formed and evolved under new global tectonic regime since Mesozoic. |
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