青藏高原东北缘循化盆地渐新世—上新世沉积相分析与沉积演化

张楗钰; 张克信; 季军良; 骆满生; 陈奋宁; 徐亚东; 王岳明

doi:10.3799/dqkx.2010.091

Volume 35 Issue 5

Sep. 2010

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Article Navigation > Earth Science > 2010 > 35(5): 774-788

ZHANG Jian-yu, ZHANG Ke-xin, JI Jun-liang, LUO Man-sheng, CHEN Fen-ning, XU Ya-dong, WANG Yue-ming, 2010. Oligocene-Pliocene Sedimentary Facies Analysis and Sedimentary Evolution of Xunhua Basin in Northeastern Margin of Qinghai-Tibet Plateau. Earth Science, 35(5): 774-788. doi: 10.3799/dqkx.2010.091

Citation:

ZHANG Jian-yu, ZHANG Ke-xin, JI Jun-liang, LUO Man-sheng, CHEN Fen-ning, XU Ya-dong, WANG Yue-ming, 2010. Oligocene-Pliocene Sedimentary Facies Analysis and Sedimentary Evolution of Xunhua Basin in Northeastern Margin of Qinghai-Tibet Plateau. Earth Science, 35(5): 774-788. doi: 10.3799/dqkx.2010.091

Citation:

ZHANG Jian-yu, ZHANG Ke-xin, JI Jun-liang, LUO Man-sheng, CHEN Fen-ning, XU Ya-dong, WANG Yue-ming, 2010. Oligocene-Pliocene Sedimentary Facies Analysis and Sedimentary Evolution of Xunhua Basin in Northeastern Margin of Qinghai-Tibet Plateau. Earth Science, 35(5): 774-788. doi: 10.3799/dqkx.2010.091

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Oligocene-Pliocene Sedimentary Facies Analysis and Sedimentary Evolution of Xunhua Basin in Northeastern Margin of Qinghai-Tibet Plateau

doi: 10.3799/dqkx.2010.091

ZHANG Jian-yu^{1, 2
,},
ZHANG Ke-xin^{1, 2
,
,},
JI Jun-liang^{1, 2},
LUO Man-sheng^{1, 2},
CHEN Fen-ning³,
XU Ya-dong^{1, 2},
WANG Yue-ming⁴

1.
Key Laboratory of Biogeology and Environmental Geology of Ministry of Education, China University of Geosciences, Wuhan 430074, China
2.
Faculty of Earth Sciences, China University of Geosciences, Wuhan 430074, China
3.
Xi'an Institute of Geology and Mineral Resources, Xi'an 710054, China
4.
Gansu Bureau of Geology and Mineral Exploration and Development, Lanzhou 730000, China

Received Date: 2010-05-31
Publish Date: 2010-09-01

Abstract

Abstract

The measured section in the southern margin of Xunhua basin located at Yangjuangongbai-Xigoushangzhuang Village, Jishi Town, Xunhua County, Qinghai Province, consists of Miocene to Pliocene strata, named as Tala Fm., Xianshuihe Fm. (consisting of Zhongzhuang Mem., Shangzhuang Mem. and Dongxiang Mem.) and Linxia Fm. (consisting of Liushu Mem. and Hewangjia Mem.). The detailed research of sedimentary facies indicates that the depositional system of the section consists of alluvial fan facies (Tala Fm.), salt water lacustrine facies and delta front facies (Xianshuihe Fm.), lacustrine facies and delta front facies with underwater fan facies (Linxia Fm.) from bottom to top. Paleocurrent measurements obtained from the imbricated structures and cross-beddings show that the paleocurrent direction of section was SE-NW, except the Linxia Fm.. The sedimentary origin analysis demonstrates that the northern margin of the western Qinling thrust belt and the south margin of the Lajishan thrust belt had uplifted as denudation areas and provided deposits to the Xunhua basin. On the contrary, during the depositional stage of the Linxia Fm., the paleocurrent was NWW, indicating that the Jishi Mountain of the eastern edge of Xunhua basin had uplifted as a main denudation area during the Late Miocene-Pliocene. The results of the grain size probability accumulative curves and C-M patterns accord with the division of sedimentary facies mentioned above, and indicate that some tractive current developed in delta front facies and underwater fan facies.
- Xunhua basin,
- sedimentary facies,
- paleocurrent,
- provenance analysis,
- grain size analysis

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