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Sedimentary environment of the Dajin conglomerate in Tibet, age of foraminiferan assemblages and their tectonic significance
Yan, Z; Fang, AM; Pan, YS; Li, JL; Liu, XH; Yu, LJ; Zhang, BG
发表日期2005
ISSN1002-0071
起始页码1014
结束页码1020
卷号15期号:11页码:2755-2760
英文摘要The Dajin conglomerate, which is one of the most important sedimentary successions of the Xigaze forearc basin in Tibet, China, consists of deep-shallow marine tuffaceous turbidites and elastic rocks bearing Nummulites, Assilina, Alveolina and Lockhartia. These fossils are very similar to the foraminiferan in the Jialazi and Maila conglomerates, and those in Gangba and Dingri areas. They developed in the Eocene. By analyzing the spatial variation of Eocene sedimentary environments of Tibet Plateau and the foraminiferan in the Dajin conglomerate, we found that Eocene sedimentation should take place on both sides of the Yarlung Tsangpo suture, and the late Eocene tectonic uplifting should make the forearc basin expose out of the sea level and begin to receive normarine deposits.
关键词TSANGPO SUTURE ZONEFORE-ARC BASINCOLLISIONINDIAEVOLUTIONASIA
英文关键词Dajin conglomerate; marine deposits; Eocene foraminiferan; Yarlung Tsangpo suture
语种英语
WOS研究方向Materials Science ; Science & Technology - Other Topics
WOS类目Materials Science, Multidisciplinary ; Multidisciplinary Sciences
WOS记录号WOS:000234606500008
来源期刊PROGRESS IN NATURAL SCIENCE
来源机构中国科学院青藏高原研究所
文献类型期刊论文
条目标识符http://gcip.llas.ac.cn/handle/2XKMVOVA/450
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GB/T 7714
Yan, Z,Fang, AM,Pan, YS,et al. Sedimentary environment of the Dajin conglomerate in Tibet, age of foraminiferan assemblages and their tectonic significance[J]. 中国科学院青藏高原研究所,2005,15(11):2755-2760.
APA Yan, Z.,Fang, AM.,Pan, YS.,Li, JL.,Liu, XH.,...&Zhang, BG.(2005).Sedimentary environment of the Dajin conglomerate in Tibet, age of foraminiferan assemblages and their tectonic significance.PROGRESS IN NATURAL SCIENCE,15(11),2755-2760.
MLA Yan, Z,et al."Sedimentary environment of the Dajin conglomerate in Tibet, age of foraminiferan assemblages and their tectonic significance".PROGRESS IN NATURAL SCIENCE 15.11(2005):2755-2760.
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