WANG Jing, WANG Hua, CHEN Si, GAN Huajun, LIU Xiaolong, LV Zhenyu, MEI Binbo, REN Jinfeng. CONTROL OF PALAEOGEOMORPHOLOGY ON SEDIMENTARY SYSTEM DISTRIBUTION: AN EXAMPLE FROM QINGXI DEPRESSION, JIUQUAN BASIN[J]. Marine Geology Frontiers, 2012, 28(3): 25-33.
Citation: |
WANG Jing, WANG Hua, CHEN Si, GAN Huajun, LIU Xiaolong, LV Zhenyu, MEI Binbo, REN Jinfeng. CONTROL OF PALAEOGEOMORPHOLOGY ON SEDIMENTARY SYSTEM DISTRIBUTION: AN EXAMPLE FROM QINGXI DEPRESSION, JIUQUAN BASIN[J]. Marine Geology Frontiers, 2012, 28(3): 25-33.
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CONTROL OF PALAEOGEOMORPHOLOGY ON SEDIMENTARY SYSTEM DISTRIBUTION: AN EXAMPLE FROM QINGXI DEPRESSION, JIUQUAN BASIN
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WANG Jing1,2,
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WANG Hua2,
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CHEN Si1,2,
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GAN Huajun2,
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LIU Xiaolong1,2,
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LV Zhenyu3,
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MEI Binbo1,2,
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REN Jinfeng1,2
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1 Key Laboratory of Tectonics and Petroleum Resources, Ministry of Education, China University of Geosciences, Wuhan 430074, China;
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2 Faculty of Earth Resources, China University of Geosciences, Wuhan 430074, China;
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3 Institute of Exploration and Development, China National Offshore Oil Corporation Tianjin Branch, Tianjin 300452, China
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Abstract
Palaeogeomorphological units, such as paleo-bulges, paleo-sags and paleo-valleys, are critical in controlling the formation and development of sedimentary systems and sequences. Sediments move through paleo-valleys (usually structural slope-break zones) and are finally deposited in paleo-sags as fan deltas and/or turbidite fans. Therefore, palaeogeomorphology research can help reveal the spatial distribution of depression and deposition centers for predicting sand-rich sedimentary systems so as to benefit the exploration of oil and gas in petroliferous basins. Balanced cross section has been widely applied in recent years as an efficient tool for study of tectonic evolution. In this paper, we used the balanced cross section technique to reestablish the palaeogeomorphological framework, taking the nose-like structure in Xiagou Formation of Lower Cretaceous in Yaxi area, Qingxi sag as an example, where fan delta, lacustrine and gravity flow depositional systems are well developed. The influence of palaeogeomorphology on sedimentary system was discussed in details.
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