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Abstracts of Acta Geologica Sinica (Chinese Edition)

Abstracts of Acta Geologica Sinica (Chinese Edition) Abstracts of Acta Geologica Sinica (Chinese Edition) Vol. 76, No. 3,2002 Neogene Stratigraphy and Palaeogeography in the Wsen etr TarimBasin HA0 Yichun'. GUAN Shaozeng', YE Liushen2. HUANG Youy~~an~. U Yongchan2 and GUAN Shiqiao' (1. China WO University of Geowiences. Beijing 100083; 2. Geological Institute of Chemical Mineral Resources, Zhuozhou, Hebei 072754; 3. Northwest Bureau of Petroleum. UrUmqi. Xinjiang 830011; 4. Bureau of Coal Geology, Zhuozhou, Hebei 072752) At the end of the Oligocene. the "long-range effect" of the India-Eurasia collision terminated the l n between the T r m ik ai basin and the PalawMediterranean and the T r m basin started a ai development of continental basin. A very thick continental sequence mainly of fluvial-lacustrine facies deposited in the western T r m basin in the Neogene. T i sequence. composed ai hs mainly of clastic rocks with intercalation of evaporites. and of varying thickness with maximum of 6050 m. is classified into the Miocene Wuqia (Ulugqat) group with three formations, from bottom to top. the Keziluoyi. Anjuan and Pakabulake, and Pliocene Artux formation. The present paper dealt with specifically the age of the Keziluoyi formation based on its biota and concluded that the formation is of http://www.deepdyve.com/assets/images/DeepDyve-Logo-lg.png Acta Geologica Sinica (English Edition) Wiley

Abstracts of Acta Geologica Sinica (Chinese Edition)

Acta Geologica Sinica (English Edition) , Volume 76 (3) – Sep 1, 2002

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Publisher
Wiley
Copyright
2002 Geological Society of China
ISSN
1000-9515
eISSN
1755-6724
DOI
10.1111/j.1755-6724.2002.tb00555.x
Publisher site
See Article on Publisher Site

Abstract

Abstracts of Acta Geologica Sinica (Chinese Edition) Vol. 76, No. 3,2002 Neogene Stratigraphy and Palaeogeography in the Wsen etr TarimBasin HA0 Yichun'. GUAN Shaozeng', YE Liushen2. HUANG Youy~~an~. U Yongchan2 and GUAN Shiqiao' (1. China WO University of Geowiences. Beijing 100083; 2. Geological Institute of Chemical Mineral Resources, Zhuozhou, Hebei 072754; 3. Northwest Bureau of Petroleum. UrUmqi. Xinjiang 830011; 4. Bureau of Coal Geology, Zhuozhou, Hebei 072752) At the end of the Oligocene. the "long-range effect" of the India-Eurasia collision terminated the l n between the T r m ik ai basin and the PalawMediterranean and the T r m basin started a ai development of continental basin. A very thick continental sequence mainly of fluvial-lacustrine facies deposited in the western T r m basin in the Neogene. T i sequence. composed ai hs mainly of clastic rocks with intercalation of evaporites. and of varying thickness with maximum of 6050 m. is classified into the Miocene Wuqia (Ulugqat) group with three formations, from bottom to top. the Keziluoyi. Anjuan and Pakabulake, and Pliocene Artux formation. The present paper dealt with specifically the age of the Keziluoyi formation based on its biota and concluded that the formation is of

Journal

Acta Geologica Sinica (English Edition)Wiley

Published: Sep 1, 2002

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