新疆叶城南部“赛力亚克达坂群”及其时代的商榷

王约; 王训练; 王野

doi:10.3799/dqkx.2016.091

Volume 41 Issue 7

Jul. 2016

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Article Navigation > Earth Science > 2016 > 41(7): 1099-1109

Wang Yue, Wang Xunlian, Wang Ye, 2016. Discussion on Age of 'Sailiyakedaban Group' in Southern Yecheng, South Xinjiang, NW China. Earth Science, 41(7): 1099-1109. doi: 10.3799/dqkx.2016.091

Citation:

Wang Yue, Wang Xunlian, Wang Ye, 2016. Discussion on Age of "Sailiyakedaban Group" in Southern Yecheng, South Xinjiang, NW China. Earth Science, 41(7): 1099-1109. doi: 10.3799/dqkx.2016.091

Wang Yue, Wang Xunlian, Wang Ye, 2016. Discussion on Age of 'Sailiyakedaban Group' in Southern Yecheng, South Xinjiang, NW China. Earth Science, 41(7): 1099-1109. doi: 10.3799/dqkx.2016.091

Citation:

Wang Yue, Wang Xunlian, Wang Ye, 2016. Discussion on Age of "Sailiyakedaban Group" in Southern Yecheng, South Xinjiang, NW China. Earth Science, 41(7): 1099-1109. doi: 10.3799/dqkx.2016.091

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Discussion on Age of "Sailiyakedaban Group" in Southern Yecheng, South Xinjiang, NW China

doi: 10.3799/dqkx.2016.091

1.
College of Resource and Environmental Engineering, Guizhou University, Guiyang 550003, China
2.
School of Earth Sciences and Resources, China University of Geosciences, Beijing 100083, China

Received Date: 2015-09-30
Publish Date: 2016-07-15

Abstract

Abstract

In the Sailiyakedaban area (in West Kunlun Mountains), Yecheng, South Xinjiang, a series of coal-bearing clastic strata, distributed in the Mazha-Kangxiwa tectonic belt, is named as the Sailiyakedaban Group and considered as the Early-Middle Triassic strata. The Mazha-Kangxiwa tectonic belt is considered as the boundaries between the West Kunlun and the Karakoram plates, as well as between the Eurasian plate and the Paleo-Tethys domain, so the dating of the coal-bearing clastics in the Mazha-Kangxiwa tectonic belt is significant to the study on the tectonic and paleogeographic evolution in West Kunlun Mountains. Lithologically, the coal-bearing clastic strata can be divided into three parts: the lower part consists mainly of conglomerates, the middle part is characterized by coals, and the upper part consists mainly of pebbly sandstones. Abundant plant fossils, of 17 genus and 20 species, were collected from the middle part of the strata. The flora is predominated by Cycadophytes (25%), ferns (20%), Ginkgopsida (20%), and Confiers (15%). Similar to the Yarkant Group flora found in the West Kunlun Mountains and the margin of the Tarim basin, it shows the characteristics of both Coniopteris-Phoenicopsis flora in North China and Ptilophyllum-Conioptersis flora in South China during the Early-Middle Jurassic transition. In addition, the coal-bearing clastic deposit in the Mazha-Kangxiwa tectonic belt not only is correlated with the Yarkant Group in the stratigraphic sequences and lithostratigraphy, but also conforms to the definition of the Yarkant Group. Therefore, the stratigraphic unit "Sailiyakedaban Group" of the Early-Middle Triassic is proposed to be suspended for use and to be replaced by the Yarkant Group of the Early-Middle Jurassic.
- Yarkant Group,
- "Sailiyakedaban Group",
- plant fossil,
- lithostratigraphy,
- Early-Middle Jurassic,
- Yecheng,
- stratigraphy,
- paleontology

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Discussion on Age of "Sailiyakedaban Group" in Southern Yecheng, South Xinjiang, NW China

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