西准噶尔晚泥盆世新建岩石地层单位：塔克台组

纵瑞文; 王志宏; 龚一鸣

doi:10.3799/dqkx.2015.063

Volume 40 Issue 5

May 2015

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Article Navigation > Earth Science > 2015 > 40(5): 763-776

Zong Ruiwen, Wang Zhihong, Gong Yiming, 2015. Taketai Formation: A New Lithostratigraphic Unit of Late Devonian in Western Junggar. Earth Science, 40(5): 763-776. doi: 10.3799/dqkx.2015.063

Citation:

Zong Ruiwen, Wang Zhihong, Gong Yiming, 2015. Taketai Formation: A New Lithostratigraphic Unit of Late Devonian in Western Junggar. Earth Science, 40(5): 763-776. doi: 10.3799/dqkx.2015.063

Zong Ruiwen, Wang Zhihong, Gong Yiming, 2015. Taketai Formation: A New Lithostratigraphic Unit of Late Devonian in Western Junggar. Earth Science, 40(5): 763-776. doi: 10.3799/dqkx.2015.063

Citation:

Zong Ruiwen, Wang Zhihong, Gong Yiming, 2015. Taketai Formation: A New Lithostratigraphic Unit of Late Devonian in Western Junggar. Earth Science, 40(5): 763-776. doi: 10.3799/dqkx.2015.063

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Taketai Formation: A New Lithostratigraphic Unit of Late Devonian in Western Junggar

doi: 10.3799/dqkx.2015.063

State Key Laboratory of Biogeology and Environmental Geology, China University of Geosciences, Wuhan 430074, China

Received Date: 2014-04-30
Publish Date: 2015-05-15

Abstract

Abstract

Based on the lithological association and sedimentary environments, the clastic stratal succession around the Taketai plateau in western Junggar is named as a new lithostratigraphic unit—Taketai Formation, which was previously assigned to the Early Carboniferous Hebukehe Formation. Taketai Formation can be subdivided into two members; the lower part is made up of volcanoclastic rocks intercalated with volcanic rocks, while the upper part is characterized by normal clastic rocks, volcanoclastic rocks and calcareous clastic rocks with a few limestones, volcanic rocks and thin coal seams. The Taketai Formation overlies the Wenlock Shaerbuer Formation in angular unconformity and its top is covered with Quaternary deposits. According to conodonts and other fossils preserved in the formation, Taketai Formation is considered to be the Late Devonian. It is formed from the littoral-neritic sea to swamp in a regression background. The same time-different stratum units of the Taketai Formation include the Zhulumute and Hongguleleng formations in adjacent regions, and it was caused by the Late Devonian marine transgression and regression from west to east in the study area.
- Taketai Formation,
- Late Devonian,
- lithostratigraphic unit,
- Hebukehe Formation,
- Hongguleleng Formation,
- western Junggar,
- stratigraphy,
- sedimentology

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References(69)

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Taketai Formation: A New Lithostratigraphic Unit of Late Devonian in Western Junggar

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