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DISCOVERY OF PARAMORPH OF HIGH-QUARTZ IN THE STRATOTYPE SECTION OF THE PERMIAN-TRIASSIC BOUNDARY AT MEISHAN OF CHANGXING; ZHEJIANG; AND ITS SIGNIFICANCE
He JW(何锦文); Chai ZF(柴之芳); Ma SL(马淑兰)
1989
发表期刊Chinese Science Bulletin
期号6页码:474-477
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 P...
关键词paramorph of high quartz, P/T boundary, Zhejiang, volcanic eruption.
资助项目Project partly supported by the National Natural Science Foundation of China.
文献类型期刊论文
条目标识符http://ir.ihep.ac.cn/handle/311005/214995
专题院士
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GB/T 7714
He JW,Chai ZF,Ma SL. DISCOVERY OF PARAMORPH OF HIGH-QUARTZ IN THE STRATOTYPE SECTION OF THE PERMIAN-TRIASSIC BOUNDARY AT MEISHAN OF CHANGXING; ZHEJIANG; AND ITS SIGNIFICANCE[J]. Chinese Science Bulletin,1989(6):474-477.
APA 何锦文,柴之芳,&马淑兰.(1989).DISCOVERY OF PARAMORPH OF HIGH-QUARTZ IN THE STRATOTYPE SECTION OF THE PERMIAN-TRIASSIC BOUNDARY AT MEISHAN OF CHANGXING; ZHEJIANG; AND ITS SIGNIFICANCE.Chinese Science Bulletin(6),474-477.
MLA 何锦文,et al."DISCOVERY OF PARAMORPH OF HIGH-QUARTZ IN THE STRATOTYPE SECTION OF THE PERMIAN-TRIASSIC BOUNDARY AT MEISHAN OF CHANGXING; ZHEJIANG; AND ITS SIGNIFICANCE".Chinese Science Bulletin .6(1989):474-477.
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