| 震旦系地质年代学新研究 |
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| 引用本文： | 胡世玲,劳秋元.震旦系地质年代学新研究[J].地质科学,1991,0(4):325-336. |
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| 作者姓名： | 胡世玲 劳秋元 |
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| 作者单位： | 1. 中国科学院地质研究所, 北京 100029;2. 同济大学海洋地质系, 上海 200092 |
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| 摘 要： | 在研究中国南方震旦系的基础上,近年来对长江峡东、滇东、皖南、赣西北、川西等震旦系典型剖面及有关花岗岩体进行了系统的地质年代学研究,并参照收集到的年龄资料,对震旦系顶、底界线和分统界线年龄作了综合研究,并提出了震旦系新的地质年代表。
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| 关 键 词： | 震旦系 同位素年龄 地质年表 |
| 收稿时间： | 1991-01-01 |
| 修稿时间： | 1991-01-01; |
NEW GEOCHRONOLOGY OF SINIAN SYSTEM |
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| Hu Shiling Liu Hongyun.NEW GEOCHRONOLOGY OF SINIAN SYSTEM[J].Chinese Journal of Geology,1991,0(4):325-336. |
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| Authors: | Hu Shiling Liu Hongyun |
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| Institution: | 1. Institute of Geology, Academic Sinica, Beijing 100029;2. Department of Marine Geology, Tongji University, Shanghai 200092 |
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| Abstract: | On the basis of previous studies on the Sinian system in southern China during the last decades, the authors, using 40Ar/39Ar dating teachnique, Rb-Sr whole rock and K-Ar methods, systematically determined a large number of samples collected from several typical Sinian sections and related granitic intrusions in eastern Yangtze Gorge area, southern Anhui, northwestern Jiangxi and western Sichuan. With the reference to the available data, a comprehensive study on the geochronology of Sinian system enables us to propose that the age of the bottom boundary of Sinian system is 900?20 Ma; the boundary between Lower and Upper Sinian is 740?40 Ma; the boundary between Sinian and Cambrian is 600?10 Ma. And a geochronological scale of the Sinian system is geven in this paper. |
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| Keywords: | Sinian Isotopic age Geochronologial scale |
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