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

	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; MA, SL
	1989
发表期刊	CHINESE SCIENCE BULLETIN
ISSN	1001-6538
卷号	34 期号:6 页码:474-477
文献类型	期刊论文
条目标识符	http://ir.nigpas.ac.cn/handle/332004/1340
专题	中国科学院南京地质古生物研究所
推荐引用方式 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,1989,34(6):474-477.
APA	HE, JW ,CHAI, ZF,&MA, SL.(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,34(6),474-477.
MLA	HE, JW ,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 34.6(1989):474-477.