川东地区黄龙组层序-岩相古地理特征
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Sequence and Lithofacies-palaeogeography Characteristics of Huanglong Formation in Easten Sichuan Basin
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    摘要:

    石炭系黄龙组作为川东天然气的主力产层之一,一直是川东地区天然气重点勘探开发层位,但该层位的沉积相特征研究较薄弱,已成为制约该地区石炭系天然气滚动勘探的因素之一。本文根据岩心描述、实测野外剖面和室内镜下岩石薄片鉴定,并结合岩石学、古生物及测井等沉积相标志的综合研究,认为黄龙组沉积发育有萨勃哈、有障壁海岸和陆棚三个沉积体系,具水体逐渐加深和范围向陆上超和扩大的海侵序列,根据沉积相标志又可进一步细分为8个亚相和13个微相,并深入讨论了黄龙组沉积期后受云南运动影响所发生的古岩溶作用和岩溶地貌特征。根据沉积相和岩溶地貌单元的划分,编制黄龙组一段(C2hl1)、黄龙组二段(C2hl2)、黄龙组三段(C2hl3)岩相古地理图,讨论了古暴露面岩溶地貌单元的展布特征与演化规律及其与储层发育的关系。

    Abstract:

    Huanglong Formation in eastern Sichuan is the major stratum of natural gas exploration and development.But sedimentary facies research in this formation is weak,it has become a factor which restricts the sequential natural gas exploration.Based on drilling core description,field profile actual measurement,slice identify,and combine the feature of sedimentary facies in petrology, palaeobiology, well logging, Huanglong Formation has been ploted? as three types of sedimentary system,including sabkha, barrier coast and continental shelf, , the sea level heighten gradually, area onlap forward the ancient land and expansile transgression sequence, according to the feature of sedimentary, Huanglong formation can be recognized as 8 subfacies and 13 microfacies, the characteristic of karst landform in Huanglong Formation, which has been impact by Yunnan Movement,is discussed. Based on the plot of sedimentary facies and karst landform, the lithofacies-palaeogeography map of Huanglong Formation each section and karst physiognomy,and it’s relationship with reservoir growth are described.

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陈浩如,郑荣才,李伟,朱宜新,徐发波,文华国.2011.川东地区黄龙组层序-岩相古地理特征[J].地质学报,85(2):246-255.
Chen hao ru, zheng rong cai, li wei, Zhu yixin, Xu fabo, wen huaguo.2011. Sequence and Lithofacies-palaeogeography Characteristics of Huanglong Formation in Easten Sichuan Basin[J]. Acta Geologica Sinica,85(2):246-255.

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  • 收稿日期:2009-09-06
  • 最后修改日期:2010-01-08
  • 录用日期:2010-01-19
  • 在线发布日期: 2011-02-11
  • 出版日期: