| 四川盆地早寒武世龙王庙期沉积特征与古地理 |
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| 引用本文： | 马腾,谭秀成,李凌,曾伟,金民东,罗冰,洪海涛,胡平.四川盆地早寒武世龙王庙期沉积特征与古地理[J].沉积学报,2016,34(1):33-48. |
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| 作者姓名： | 马腾 谭秀成 李凌 曾伟 金民东 罗冰 洪海涛 胡平 |
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| 作者单位： | 1.西南石油大学油气藏地质及开发工程国家重点实验室 成都 610500; |
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| 基金项目： | 国家自然科学基金，国家科技重大专项，四川省省属高校"天然气地质"科研创新团队建设计划 |
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| 摘 要： | 基于盆内及其周缘钻孔取芯和露头剖面资料,结合区域背景和龙王庙组地层充填厚度分析认为,四川盆地周缘龙王庙期北邻摩天岭微古陆和汉南古陆、西接康滇古陆,东南和东北分别为威信-黔江、石阡-秀山-龙山和镇巴-巫溪-巴东水下古隆起环抱;盆内呈近北东向展布的川中古隆起和阆中-通江坳陷、江津-奉节坳陷构成“一隆两坳”,南部泸州-筠连-昭通继承性坳陷依然存在;盆地及周缘向东北隅和东南隅分别接入秦岭洋和江南盆地。受此影响,龙王庙期发育连陆碳酸盐岩台地-斜坡-盆地沉积体系,连陆碳酸盐岩台地构成沉积主体,可识别出混积潮坪、局限-蒸发台地、半局限-局限台地和台地边缘沉积相类型;进一步通过碎屑岩含量与陆源方向、石灰岩、白云岩和膏盐岩含量与海域局限性和台地边缘相对位置、颗粒岩含量等分析,阐明了龙王庙期岩相古地理展布样式并建立了沉积模式。结果表明潮坪向海侧、水下古隆起、泸州-筠连-昭通坳陷周缘是颗粒滩有利发育区,乐山和资阳地区经由早寒武世早期的充填拼合作用已形成统一古隆起,震旦纪末期-早寒武世的南北向桐梓-筠连裂陷槽演变为泸州-筠连-昭通台内坳陷,研究成果对拓宽龙王庙组滩控岩溶型储层的勘探领域具有重要的指导作用。
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| 关 键 词： | 颗粒滩 古隆起 连陆碳酸盐岩台地 台地边缘 相模式 古地理格局 |
| 收稿时间： | 2015-01-19 |
Sedimentary Characteristics and Lithofacies Palaeogeography during Longwangmiao Period of Early Cambrian,Sichuan Bain |
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| Institution: | 1.Key Laboratory of Natural Gas Geology, Southwest Petroleum University, Chengdu 610500, China;2.The Sedimentary and Accumulation Department of Key Laboratory of Carbonate Reservoirs, PetroChina, Southwest Petroleum University, Chengdu 610500, China;3.College of Resource and Environment, Southwest Petroleum University, Chengdu 610500, China;4.PetroChina Sichuan & Chuanqing Drilling Engineering Corporation, Chengdu 610000, China |
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| Abstract: | In order to improve the understanding on the sedimentary characteristics and lithofacies palaeogeography in the Lower Cambrian Longwangmiao Formation of the Sichuan Basin and its adjacent regions, a relative comprehensive analysis on the boreholes and outcrops data were performed. Particularly, by examining the regional geological settings and the thickness distribution pattern within Longwangmiao Fromation, this paper found that the Sichuan Basin and its adjacent areas are bordered by Motianling Micro-oldland and Hannan Oldland in the north, Kangdian Oldland in the west. In the southeast and northeast regions within the study area, were embraced by underwater palaeouplift named Weixin-Qianjiang, Shiqian-Xiushan-Longshan and Zhenba-Wuxi-Badong respectively. Within the present basin, Central Sichuan palaeouplift, and depressins of Langzhong-Tongjiang, Jiangjin-Fengjie constitute of the palaeogeographic pattern of "one uplift and two depressions", while in the south an inherited depression region named "Luzhou-Junlian-Zhaotong" still existed. To the northeast and southwest corner, Qinling ocean and Jiangnan Basin are connected. Strikingly impacted by the palaeogeographic pattern, a land-tied carbonate platform was found to cover the main body of the Sichuan Basin within the platform-ramp-basin sedimentary system, which may further be divided into mixed tidal flat, restricted to evaporate platform, semi-restricted to restricted platform and platform margin. Furtherly, by analyzing the terrigenous clasts content and its direction, the content distribution pattern of limestone, dolostone and gyprock elucidating the waters localization and the relative locations of the platform margin, and the grain-shoal content, it clarifies the distribution pattern of the lithofacies paleogeography during Longwangmiao period, establishing the sedimentary model successively. The results indicate that, the open ocean side of the flat tidal, underwater palaeouplift and the periphery areas of Luzhou-Junlian-Zhaotong are preferable zones for grain shoal development. The filling and joining during the early stage of early Cambrian results in a unified palaeouplift in Leshan and Ziyang, while the north-south staphrogenic Trough in Tongzi-Junlian during the end of Ediacaran and Early Cambrian turned into the Luzhou-Junlian-Zhaotong depression within the platform. Two depression zones in the south have been verified by drilling holes of Well Dengtan 1 and Well Taihe 1. The results may help to guide and broaden the exploration field of karstificated grain-shoal reservoir study. |
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| Keywords: | grain shoal palaeouplift land-tied carbonate platform platform margin depositional model palaeogeographic pattern |
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