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The Late Triassic Sequence‐Stratigraphic Framework of the Upper Yangtze Region, South China
Author(s) -
MEI Mingxiang,
LIU Shaofeng
Publication year - 2017
Publication title -
acta geologica sinica ‐ english edition
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 0.444
H-Index - 61
eISSN - 1755-6724
pISSN - 1000-9515
DOI - 10.1111/1755-6724.13063
Subject(s) - geology , foreland basin , paleontology , fluvial , orogeny , facies , early triassic , structural basin , siliciclastic , geomorphology , permian
In the transitional period between the Middle and the Late Triassic, the Indochina orogeny caused two tectonic events in South China: (1) the formation and uplift of the Qinling‐Dabie orogenic belt along the northern margin of the South China Plate, due to its collision with the North China Plate; and 2) the development of a 1300‐km‐wide intra‐continental orogen in the southeastern part of the South China Plate, which led to a northwestward movement of the foreland thrust‐fold zone. These tectonic events resulted in the ending of the Yangtze Platform, and were a stable paleogeographic factor from the Eidacaran to the end of the Middle Triassic. This platform was characterized by the widespread development of shallow‐water carbonates. After the end of the Yangtze Platform, the upper Yangtze foreland basin (or Sichuan foreland basin) was formed during the Late Triassic and became a accumulation site of fluvial deposits that are composed of related strata of the Xujiahe Formation. In western Sichuan Province, the Xujiahe Formation overlies the Maantang Formation shallow‐water carbonate rocks of the Xiaotangzi Formation siliciclastic rocks (from shelf shales to littoral facies). The sequence‐stratigraphic framework of the Upper Triassic in the upper Yangtze foreland basin indicates a particular alluvial architecture, characterized by sequences composed of (1) successions of low‐energy fluvial deposits of high‐accommodation phases, including coal seams, and (2) high‐energy fluvial deposits of low‐accommodation phases, including amalgamated river‐channel sandstones. The spatial distribution of these fluvial deposits belonging to the Xujiahe Formation and its relative strata is characterized by gradual thinning‐out, overlapping, and pinching‐out toward both the east and south. This sedimentary record therefore expresses a particular sequence‐stratigraphic succession of fluvial deposits within the filling succession of the foreland basin. The sequence‐stratigraphic framework for the Upper Triassic in the Upper Yangtze region provides a record of the end of the Yangtze Platform and the formation of the upper Yangtze foreland basin.