| “福建-岭南地块”质疑 |
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| 引用本文： | 杨志坚,陈玉华.“福建-岭南地块”质疑[J].地质科学,1984,0(3):244-252. |
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| 作者姓名： | 杨志坚 陈玉华 |
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| 作者单位： | 中国地质科学院南京地质矿产研究所 |
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| 摘 要： | 亚洲大多数地质学家认为,渤海、东海、黄海和日本海等海域,是新生代逐渐形成的。这样,就有理由认为,今天的我国东部大陆与朝鲜半岛和日本列岛,在前新生代的地质构造发展,是一脉相连的。关于它们之间的连接图式,日本地质学家小林贞一,在三十年代初曾提出“秦岭-汉城地轴”,五十年代初又提出“福建-岭南地块”之说。
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| 关 键 词： | , |
| 收稿时间： | 1983-01-31 |
| 修稿时间： | 1983-01-31; |
SOME QUERIES CONCERNNING "FUJIAN-LINGNAN BLOCK" |
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| Yang Zhijian,Chen Yuhua.SOME QUERIES CONCERNNING "FUJIAN-LINGNAN BLOCK"[J].Chinese Journal of Geology,1984,0(3):244-252. |
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| Authors: | Yang Zhijian Chen Yuhua |
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| Institution: | Nanjing Institute of Geology and Mineral Resouces, Chinese Academy of Geological Sciences, Nanjing |
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| Abstract: | The pattern of "Pujian-Lingnan Block" linked by "Fujian Block" and "Lingnan Block" across a sea was suggested by T. Kobayashi in the beginning of 1950s and was then continuously used by many geologists. The author consideres preliminarily that this pattern is inconsistent with the facts in the light of the information of continental and marine geology and geophysics and analytical method of historical tectonics. The geological features of Okchon Depression in South Korea and "Lingnan Block" are very similar to the palaeodepression of Northern Jiangsu and Nanjing-Zhenjiang Uplift and were linked each other.In accordance with deep structure, palaeotectonic lineament, great deep fault, stratigraphy and palaeontology, geology of island and reef along the coast, folding episode, second grade synclinoria and antisynclinoria as well as magmatic rock type and ore attribution, the author believes that the geological features and tectonic development of Taihu-Shanghai-Qiantong-East Zhejiang can be closely linked with those of the Southwest Japan across the East China Sea in the Cenozoic Era. |
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| Keywords: | , |
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