南襄盆地泌阳凹陷深水湖底扇厘定及碎屑锆石U-Pb年代学物源追踪

张建光; 姚光庆; 陈亚兵; 樊中海; 林社卿; 杨永利

doi:10.3799/dqkx.2011.116

Volume 36 Issue 6

Jun. 2011

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ZHANG Jian-guang, YAO Guang-qing, CHEN Ya-bing, FAN Zhong-hai, LIN She-qing, YANG Yong-li, 2011. Sub-Lacustrine Fan of Chengdian and Zircon U-Pb Ages and Constraint on Its Provenance in Biyang Depression, Nanxiang Basin, China. Earth Science, 36(6): 1105-1118. doi: 10.3799/dqkx.2011.116

Citation:

ZHANG Jian-guang, YAO Guang-qing, CHEN Ya-bing, FAN Zhong-hai, LIN She-qing, YANG Yong-li, 2011. Sub-Lacustrine Fan of Chengdian and Zircon U-Pb Ages and Constraint on Its Provenance in Biyang Depression, Nanxiang Basin, China. Earth Science, 36(6): 1105-1118. doi: 10.3799/dqkx.2011.116

Citation:

ZHANG Jian-guang, YAO Guang-qing, CHEN Ya-bing, FAN Zhong-hai, LIN She-qing, YANG Yong-li, 2011. Sub-Lacustrine Fan of Chengdian and Zircon U-Pb Ages and Constraint on Its Provenance in Biyang Depression, Nanxiang Basin, China. Earth Science, 36(6): 1105-1118. doi: 10.3799/dqkx.2011.116

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Sub-Lacustrine Fan of Chengdian and Zircon U-Pb Ages and Constraint on Its Provenance in Biyang Depression, Nanxiang Basin, China

doi: 10.3799/dqkx.2011.116

1.
Faculty of Earth Resources, China University of Geosciences, Wuhan 430074, China
2.
Key Laboratory of Tectonics and Petroleum Resources of Ministry of Education, China University of Geosciences, Wuhan 430074, China
3.
Research Institute of Exploration and Development of Henan Oilfield, Branch Company of SINOPEC, Nanyang 473132, China

Received Date: 2011-01-29
Available Online: 2021-11-10
Publish Date: 2011-06-15

Abstract

Abstract

Aiming at Chengdian deep water sandstone in Biyang depression of Nanxiang basin, we analyzed the core, the particle size, thin section, heavy minerals testing materials, structure of sandbody and the geophysical response of sedimentary sandbody, and found that the sub-lacustrine fan is an isolated body with fine and coarse lithology which consists of mainly massive lithologic facies with the characteristics of sandy debris flow sediments, but wavy bedding and cross bedding lithologic facies, two lithologic facies have its own particle-size feature, which shows the feature of turbidity current and tractive current.It's controlled by the paroxysmal flood, the revolving tilted effect and a gentle slope, we define it as a flood cause sub-lacustrine fan of composite transportation. In order to trace its provenance using clastic zircons dating analysis of sandstone samples, we selected samples from Chengdian sub-lacustrine and the Houzhuang delta area. The result shows: zircons microarea apparent ages of Chengdian sub-lacustrine and Houzhuang delta mainly similarly distribute between 115Ma and 166Ma with single peak and the magmatic zircons occupy the main part, with a few metamorphic zircons. Also, there are some different type zircons distributing in the age populations of 247-210Ma, 475-412Ma, 813-663Ma and 3489-1692Ma. In combination with regional geological settings and detritus zircon ages and heavy minerals composition, the authors come to the following preliminary conclusions: the sub-lacustrine sandbody derived from Houzhuang delta and its source rocks formation period is early Cretaceous to middle Jurassic, corresponding to Yanshan tectonic stage. Moreover, the source area is mainly Yanshanian granite in Kuanping-taowan tecnoic rock facies belt, including Yanshanian metamorphic rocks and the metamorphic rocks or magmatic rocks of Prejinningian period, Jinningian period, Caledonian period and Indosinian period may offer contributions to different degree.
- sub-lacustrine fan,
- zircon U-Pb ages,
- provenance,
- Nanxiang basin,
- Biyang depression,
- sedimentation

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References(67)

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Sub-Lacustrine Fan of Chengdian and Zircon U-Pb Ages and Constraint on Its Provenance in Biyang Depression, Nanxiang Basin, China

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