引用本文:卫洪春, 牟传龙, 谭钦银, 余谦.云南思茅盆地二叠纪层序地层研究[J].沉积与特提斯地质,2003,(2):54-57.[点击复制]
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云南思茅盆地二叠纪层序地层研究
卫洪春,牟传龙,谭钦银,余谦
0
(1. 四川智强集团有限公司, 四川 达州 635000;
2. 成都地质矿产研究所, 四川 成都 610082)
摘要:
在野外实地考察和综合研究的基础上,根据层序界面特征和凝缩层,思茅盆地二叠系可分为9个Ⅲ级层序,其中下二叠统3个,上二叠统6个。根据区域特点,认为二叠纪可分为2个Ⅱ级层序,在思茅盆地范围,乃至中国南方可以进行对比。
关键词:  思茅盆地  二叠纪  层序地层  云南
DOI:
附件
投稿时间:2003-04-01
基金项目:
Sequence stratigraphy of the Permian strata in the Simao Basin, Yunnan
WEI Hong-chun, MOU Chuan-long, TAN Qin-yin, YU Qian
(1. Sichuan Zhiqiang Group Cor., Ltd., Dazhou, 635000, Sichuan, China;
2. Chengdu Institute of Geology and Mineral Resources, Chengdu 610082, Sichuan, China)
Abstract:
The Permian strata in the Simao Basin, Yunnan may be divided, on the basis of sequence boundaries and condensed horizons in combination with the field observations along the Zhendong-Dehua sections, into two second-order sequences and nine third-order sequenes including three Lower Permian sequences and six Upper Permian sequences. These sequences may be well compared both throughout the basin and even southern China, implying that a correlation can also be made in eustatic fluctuations, tectonism and sedimentary evolution in southern China.
Key words:  Simao Basin  Permian  sequence stratigraphy  Yunnan

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