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Characteristics and evolution of gravity flow deposits of the first member of Ordovician Lashizhong Formation in northwestern margin of Ordos Basin
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Chunwei JIANG, Hua LI, Youbin HE, Yiming HE, Fengnan YAO, Jize WU, Xiankun ZHANG
Journal of Palaeogeography (Chinese Edition) | 2026, 28(2) : 524 - 536
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Journal of Palaeogeography (Chinese Edition) | 2026, 28(2): 524-536
• SPECIAL TOPIC ON THE 100TH ANNIVERSARY OF PROFESSOR FENG ZENGZHAO •
Characteristics and evolution of gravity flow deposits of the first member of Ordovician Lashizhong Formation in northwestern margin of Ordos Basin
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Chunwei JIANG, Hua LI, Youbin HE, Yiming HE, Fengnan YAO, Jize WU, Xiankun ZHANG
Affiliations
  • School of Geosciences,Yangtze University, Wuhan 430100,China
  • JIANG Chunwei,born in 2001,postgraduate,is engaged in deep-water sedimentology. E-mail: .

About Author:

JIANG Chunwei,born in 2001,postgraduate,is engaged in deep-water sedimentology. E-mail: .

Published: 2026-04-01 doi: 10.7605/gdlxb.2026.038
Outline
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For the problem of unclear evolutionary process of deep-water gravity flow deposition in the first member of Ordovician Lashizhong Formation in northwestern margin of Ordos Basin,the characteristics and evolution are studied on the basis of outcrop data,microscopic observation and grain size analysis,and finally the sedimentary modles are established. The results show that: (1)five lithofacies are developed in the study area,corresponding to horizontal bedding shale facies(F1),massive bedding calcirudite facies(F2),graded bedding fine sandstone facies(F3),parallel bedding fine sandstone to siltstone facies(F4)and small-scale cross-bedding siltstone facies(F5);(2)four deep-water depositional types are identified according to the shapes and stacking styles of sandstones: complex channels deposition,migrating channels depositon,proximal lobes deposition and distal lobes deposition;(3)complex channels,lobes,migrating channels and lobes are developed vertically in sequence;and(4)gravity flow deposition can be divided into two stages. In the first stage,the energy of gravity flow is high,forming the complex channel;With energy attenuation,small-scale lobes are developed. When in the second stage,the gravity flow erupts,which the energy is lower than the gravity flow in the first stage,and migrating channel is developed. As the energy of gravity flow continues to wane,deposition becomes dominant,resulting in a vertical transition form channels to lobes,with proximal lobes and distal lobes sequentially are developing in the depositional system. This study can improve the understanding of the sedimentary evolution law of gravity flow and is helpful to deep-water oil and gas exploration.

gravity flow deposit  /  channel  /  lobe  /  turbidity current  /  Ordos Basin  /  Ordovician
姜纯伟, 李华, 何幼斌, 何一鸣, 姚凤南, 吴吉泽, 张显坤. 鄂尔多斯盆地西北缘奥陶系拉什仲组一段重力流沉积特征及演化*. 古地理学报, 2026 , 28 (2) : 524 -536 . DOI: 10.7605/gdlxb.2026.038
Chunwei JIANG, Hua LI, Youbin HE, Yiming HE, Fengnan YAO, Jize WU, Xiankun ZHANG. Characteristics and evolution of gravity flow deposits of the first member of Ordovician Lashizhong Formation in northwestern margin of Ordos Basin[J]. Journal of Palaeogeography (Chinese Edition), 2026 , 28 (2) : 524 -536 . DOI: 10.7605/gdlxb.2026.038
  • National Natural Science Foundation of China(42272113)
  • National Natural Science Foundation of China(42272115)
Year 2026 volume 28 Issue 2
153
68
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BibTeX
Article Info
doi: 10.7605/gdlxb.2026.038
  • Receive Date:2025-04-16
  • Online Date:2026-09-24
  • Published:2026-04-01
Article Data
Affiliations
History
  • Received:2025-04-16
  • Revised:2025-07-04
Funding
National Natural Science Foundation of China(42272113)
National Natural Science Foundation of China(42272115)
Affiliations
    School of Geosciences,Yangtze University, Wuhan 430100,China

Corresponding:

LI Hua,born in 1984,professor,is engaged in sedimentology. E-mail: .
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表12种不同金属材料的力学参数
科
Family
属数
Number of
genus
种数
Number of
species
占总种数比例
Percentage of
total species (%)
属
Genus
种数
Number of
species
占总种数比例
Percentage of total
species (%)
鹅膏菌科Amanitaceae 2 11 5.26 鹅膏菌属 Amanita 10 4.78
小菇科 Mycenaceae 2 12 5.74 丝盖伞属 Inocybe 5 2.39
多孔菌科 Polyporaceae 8 14 6.70 蜡蘑属 Laccaria 5 2.39
红菇科 Russulaceae 3 23 11.00 小皮伞属 Marasmius 6 2.87
小菇属 Mycena 11 5.26
光柄菇属 Pluteus 5 2.39
红菇属 Russula 17 8.13
栓菌属 Trametes 5 2.39
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