Evidence map›Paper›PMID 40659763›Full record

ArticleScientific reports2025

The source-to-sink system in continental rift lacustrine basins of the Nantun Formation in X Sag of the Tamtsag Basin, Mongolia.

Liyuan Liu, Zongbao Liu, Rongsheng Zhao, Lin Cong, Xingquan Liu, Shiwei Xin, Zihao Mu

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Article in Scientific reports, 2025. The graph could read no effect estimate from its abstract, so it casts no vote on the map. Not yet cited in PubMed.

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5 · Who and what money

Authors and funding

7 authors.

Liyuan LiuEarth Science College, Northeast Petroleum University, Daqing, 163318, China.
Zongbao LiuEarth Science College, Northeast Petroleum University, Daqing, 163318, China. lzbdqpi@163.com.
Rongsheng ZhaoEarth Science College, Jilin University, Changchun, 130061, China.
Lin CongEarth Science College, Northeast Petroleum University, Daqing, 163318, China.
Xingquan LiuInternational Exploration and Development Company, Daqing Oilfield Company Ltd, Daqing, 163000, Heilongjiang, China.
Shiwei XinPetroChina Daqing Tamsag, LLC, Daqing, 163712, Heilongjiang, China.
Zihao MuSchool of Computer and Information Technology, Northeast Petroleum University, Daqing, 163318, China.

Funding

No grant is acknowledged in the PubMed record.

6 · The paper itself

Abstract

The strata of the first member of the Nantun Formation constitute the primary targets for oil and gas exploration and development in X sag of the Tamtsag Basin. However, the distribution pattern of sand bodies within these strata remains poorly understood due to the complex interplay of factors such as provenance supply, boundary fault growth and evolution, and sediment transport pathways, which have led to diverse source-to-sink (S2S) systems. This study aims to provide a detailed characterization of these S2S systems. The results indicate the following: (1) Activity of the boundary faults within the first member of the Nantun Formation increased progressively, controlling paleovalley development and migration of the subsidence center and depocenter; (2) Three distinct S2S systems are identified in the study area: the "transverse drainage - fan delta" system, the "transverse drainage - braided delta" system, and the "axial drainage - braided delta" system, with their spatial distributions exhibiting significant inheritance; (3) Evolution of the S2S systems is governed by growth of the sag-controlling boundary faults and variations in provenance supply intensity.

Indexed as

Fault growth evolutionK1n1Provenance supply intensitySource-to-sinkTamtsag Basin

Identifiers

PMID40659763
PMCPMC12260008

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