岱海湖盆沿坡流与顺坡流相互作用的沉积响应

陈彬滔; 于兴河; 王天奇; 杨丽莎; 潘树新; 李顺利

doi:10.3799/dqkx.2014.038

Volume 39 Issue 4

Apr. 2014

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Article Navigation > Earth Science > 2014 > 39(4): 399-410

Chen Bintao, Yu Xinghe, Wang Tianqi, Yang Lisha, Pan Shuxin, Li Shunli, 2014. Sedimentary Response to Interaction between Alongslope and Downslope Currents in Daihai Lake, North China. Earth Science, 39(4): 399-410. doi: 10.3799/dqkx.2014.038

Citation:

Chen Bintao, Yu Xinghe, Wang Tianqi, Yang Lisha, Pan Shuxin, Li Shunli, 2014. Sedimentary Response to Interaction between Alongslope and Downslope Currents in Daihai Lake, North China. Earth Science, 39(4): 399-410. doi: 10.3799/dqkx.2014.038

Citation:

Chen Bintao, Yu Xinghe, Wang Tianqi, Yang Lisha, Pan Shuxin, Li Shunli, 2014. Sedimentary Response to Interaction between Alongslope and Downslope Currents in Daihai Lake, North China. Earth Science, 39(4): 399-410. doi: 10.3799/dqkx.2014.038

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Sedimentary Response to Interaction between Alongslope and Downslope Currents in Daihai Lake, North China

doi: 10.3799/dqkx.2014.038

1.
Research Institute of Petroleum Exploration and Development-Northwest (NWGI), PetroChina, Lanzhou 730020, China
2.
School of Energy Resources, China University of Geosciences, Beijing 100083, China

Received Date: 2013-07-10
Publish Date: 2014-04-15

Abstract

Abstract

In order to confirm the intensity of alongslope current in lacustrine basin and its effect on the sedimentation of delta front, the modern sedimentation of fault-depression lacustrine basin (Daihai Lake) in Inner Mongolia, North China has been explored in this study. Based on analysis of satellite images, on-site wave observation and floating ball measurement, trench excavation, sedimentary characteristics description, sample analysis, and sandbodies comparison at the framework section, it can be concluded that the steep side of Daihai lacustrine basin was dominated by the process of downslope current, where distributary channels and river mouth bar were developed with good connectivity of sandbodies in vertical, forming large set of massive sandbodies; the interaction between downslope and alongslope currents can be found in the delta front of the gentle side, where the wave-genetic lithofacies was well-developed with sandy sediments sheeted seriously, coarsening upward rhythm was not obvious in vertical sequence, sandbodies in the river mouth were distributed asymmetrically. Sandbodies in the upstream direction of alongslope drifting were distributed continuously and superposed of multi-layers, with good connectivity in lateral; in the downstream direction, muddy intercalations were well-developed, sandbodies were distributed isolatedly with strong heterogeneity.
- alongslope current,
- downslope current,
- delta,
- sedimentary response,
- sediments,
- petroleum reservoirs,
- Daihai lacustrine basin

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References(43)

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Sedimentary Response to Interaction between Alongslope and Downslope Currents in Daihai Lake, North China

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