4.6 Article

Mud-coated intraclasts: A criterion for recognizing sandy mass-transport deposits - Deep-lacustrine massive sandstone of the Upper Triassic Yanchang Formation, Ordos Basin, Central China

期刊

JOURNAL OF ASIAN EARTH SCIENCES
卷 129, 期 -, 页码 98-116

出版社

PERGAMON-ELSEVIER SCIENCE LTD
DOI: 10.1016/j.jseaes.2016.06.007

关键词

Mud-coated intraclasts; Sandy mass-transport deposits; Sandy debris flow; Yanchang Formation; Ordos Basin; Central China

资金

  1. Chinese Major National Scientific and Technological Program [2011ZX05001-003]
  2. Scientific and Technological Program of CNPC [2016B-0301]

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Numerous examples of sandy mass-transport deposits (SMTDs) in deep-marine and deep-lacustrine environments have been documented by researchers worldwide in recent years. However, it is an enormous challenge that how to distinguish the subaqueous mass-transport processes from the depositional records. After the rigorous examination of several outcrops in the Ordos lacustrine basin in central China, we propose that the mud-coated intraclasts in the deep-water thick massive sandstone of the Yanchang Formation are a viable criterion to recognize deposition from sandy debris flows in delta front environments. These so-called mud-coated intraclasts are a newly discovered special depositional phenomenon in the massive clean sandstones in China's lacustrine basins. A mud-coated intraclast generally consists of two components: an inner core and a mud coating. The inner core is generally composed of muddy blobs or sandy lumps. The mud coatings are generally composed of thin shales or mud-rich fine-grained sediments. The inner core, which is generally coated by nearly concentric ring-shaped mud coatings, is embedded in massive deep-water sandstones. Because these features have never been documented in the. geological literature, the present authors called them mud-coated intraclasts in the present study. The depositional features suggest that the sediments that contain these mud-coated intraclasts were characterized by en masse emplacement (i.e., a Bingham plastic behavior) and were supported by the strength of the plastic medium at all times (i.e., no flow transformations occurred during their transport and deposition). Accordingly, mud-coated intraclasts are one of the most significant criteria that indicate sandy debrites as the origin of the deep-water thick massive sandstones in the Yanchang Formation. This diagnostic feature may be useful to identify analogous SMTDs in other locations. (C) 2016 Elsevier Ltd. All rights reserved.

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