• 石油勘探與開發:英文版 · 2020年第2期292-305,共14頁

    Origin and depositional characteristics of supported conglomerates

    作者:ZHANG Changmin,SONG Xinmin,WANG Xiaojun,WANG Xulong,ZHAO Kang,SHUANG Qi,LI Shaohua

    摘要:The origin and depositional characteristics of supported conglomerates in the Mahu Sag, Junggar Basin, Xinjiang, China, are examined. Based on the terminological comparison, modern sedimentary survey and core description, the initial connotation and similarities and differences in definition between supported conglomerates and other similar concepts are discussed, the modern sedimentary environment in which supported conglomerates develop is analyzed, and the sedimentological characteristics of supported conglomerates formed in different depositional environments revealed by the cores of Mahu conglomerate oil field in the Junggar Basin are described. The supported conglomerate is similar in texture to grain supported conglomerate and openwork conglomerate but has differences from them, so it is suggested to keep the term "supported conglomerate", but the formation mechanism of supported conglomerate needs to be re-examined. Through field survey of modern sediments in Baiyanghe alluvial fan, Huangyangquan alluvial fan, and Wulungu Lake in Xinjiang, it is found that supported gravels not only formed by flooding events but also by sieving, avalanching, fluvial sorting as well as wind and wave reworking in the depositional environments such as inter-mountain creek, colluvium fan, gravel channel on gobi and the fan surface, lake beach, delta front, subaerial debris flow and subwater grain-flow etc. Supported gravels could form supported conglomerate after being buried. Supported conglomerates of seven different origins have been recognized in the cores of the Triassic and Permian stratum of Mahu Depression, Junggar Basin, namely, supported conglomerates in gravel channel deposits, in wind reworked channel deposits, in gravel beach bar deposits, in wave reworked delta front deposits, in mouth bar deposits and in debris flow deposits respectively. The study shows the supported conglomerates may be formed by a single depositional event or by multi-events during the post-depositional sedimentary reworking and even in diag

    發文機構:School of Geosciences PetroChina Research Institute of Petroleum Exploration&Development PetroChina Xinjiang Oilfield Company

    關鍵詞:supportedconglomerateopenworkconglomerategrainsupportedconglomeraterocktexturesedimentaryenvironmentandfaciesreservoirrockconglomeratereservoirMahudepression

    分類號: P618.13[天文地球—礦床學]

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