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拉巴灰岩:深水碳酸盐沉积成因的认识及其意义
周志澄1; 郭震宇1; 王玉净1; 方宗杰1; 肖荫文2
2000
Source Publication地层学杂志
ISSN0253-4959
Volume24.0Issue:003Pages:190-194
Abstract滇西二叠系拉巴组中的拉巴灰岩的成因长期以来曾引起广泛争议。对拉巴灰岩的产状、结构构造及碳酸盐微相特征的研究表明,拉巴灰岩最初形成于浅水碳酸盐台地,由于突发的地质事件,被搬运至深水,半深水环境中沉积下来,拉巴灰岩的出现,证明在二叠纪,昌宁-孟连洋盆与相邻的陆棚之间,有陡峻的陆棚边棱存在。
Keyword二叠系 拉巴灰岩 深水-半深水沉积 碳酸盐沉积
Indexed ByCSCD
Language中文
CSCD IDCSCD:554045
Document Type期刊论文
Identifierhttp://ir.nigpas.ac.cn/handle/332004/38935
Collection中国科学院南京地质古生物研究所
Affiliation1.中国科学院南京地质古生物研究所
2.云南省地质矿产局区域地质矿产调查大队
First Author Affilication中国科学院南京地质古生物研究所
Recommended Citation
GB/T 7714
周志澄,郭震宇,王玉净,等. 拉巴灰岩:深水碳酸盐沉积成因的认识及其意义[J]. 地层学杂志,2000,24.0(003):190-194.
APA 周志澄,郭震宇,王玉净,方宗杰,&肖荫文.(2000).拉巴灰岩:深水碳酸盐沉积成因的认识及其意义.地层学杂志,24.0(003),190-194.
MLA 周志澄,et al."拉巴灰岩:深水碳酸盐沉积成因的认识及其意义".地层学杂志 24.0.003(2000):190-194.
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