DISCOVERY OF PARAMORPH OF HIGH-QUARTZ IN THE STRATOTYPE SECTION OF THE PERMIAN-TRIASSIC BOUNDARY AT MEISHAN OF CHANGXING, ZHEJIANG, AND ITS SIGNIFICANCE

被引：1
|
作者：
何锦文
柴之芳
马淑兰
机构：
[1] Academia Sinica
[2] Institute oF High Energy Physics
[3] NanJing Institute of Geology and Paleontology
[4] Beijing
来源：
ChineseScienceBulletin | 1989年 / 06期
基金：
中国国家自然科学基金;
关键词：
paramorph of high quartz; P/T boundary; Zhejiang; volcanic eruption;
D O I：
暂无
中图分类号：
学科分类号：
摘要：
Section Z of Meishan in Changxing of Zhejiang, known as the stratotype section of the Permain-Triassic boundary in South China, is also one of the candidate stratotype sections of the same boundary in the world. Here the strata crossing the Permian-Triassic boundary are well exposed. The Upper Permian Changhsingian is composed
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页码：474 / 477
页数：4
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