磨溪气田嘉二段陆表海碳酸盐岩台地内滩体发育规律

谭秀成

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磨溪气田嘉二段陆表海碳酸盐岩台地内滩体发育规律

谭秀成

文章导航 > 沉积学报 > 2009 > 27(5): 995-1001

谭秀成. 磨溪气田嘉二段陆表海碳酸盐岩台地内滩体发育规律[J]. 沉积学报, 2009, 27(5): 995-1001.

引用本文:

谭秀成. 磨溪气田嘉二段陆表海碳酸盐岩台地内滩体发育规律[J]. 沉积学报, 2009, 27(5): 995-1001.

TAN Xiucheng. Shoal Development within the Epicontinental Carbonate Platform, Jia 2 Member, Lower Triassic, Moxi Gas Field, Central Sichuan Basin[J]. Acta Sedimentologica Sinica, 2009, 27(5): 995-1001.

Citation:

TAN Xiucheng. Shoal Development within the Epicontinental Carbonate Platform, Jia 2 Member, Lower Triassic, Moxi Gas Field, Central Sichuan Basin[J]. Acta Sedimentologica Sinica, 2009, 27(5): 995-1001.

谭秀成. 磨溪气田嘉二段陆表海碳酸盐岩台地内滩体发育规律[J]. 沉积学报, 2009, 27(5): 995-1001.

引用本文:

谭秀成. 磨溪气田嘉二段陆表海碳酸盐岩台地内滩体发育规律[J]. 沉积学报, 2009, 27(5): 995-1001.

Citation:

磨溪气田嘉二段陆表海碳酸盐岩台地内滩体发育规律

谭秀成

西南石油大学资源与环境学院成都610500

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谭秀成

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Shoal Development within the Epicontinental Carbonate Platform, Jia 2 Member, Lower Triassic, Moxi Gas Field, Central Sichuan Basin

TAN Xiucheng

.School of Resource and Environment, Southwest Petroleum University, Chengdu610500;

More Information

Corresponding author: TAN Xiucheng

摘要

摘要: 近年来，四川盆地三叠系台缘鲕滩的油气勘探取得了重大的突破和进展，激发了人们对广阔台地内部滩体的研究兴趣。以四川盆地川中地区磨溪气田嘉二2A层为研究对象，通过对区内钻孔的测、录井及岩心芯资料的分析，总结了陆表海碳酸盐岩台地上台内滩体发育特征：向上变浅序列发育、单滩体厚度一般小于4 m、累积厚度较小以及横向连续性较差。进一步分析讨论后认为，沉积期古地貌、古水深、海水动荡程度以及古海平面相对升降变化共同控制了台内滩的发育与分布，结果表明陆表海碳酸盐岩台地内继承性古隆起是台内滩体的有利发育区，形成的台内滩体具有一定的厚度规模和较大分布面积，但是台地内部的隆坳地形分异使滩体横向分布变化较大。这些认识可为台内鲕滩储层的下一步勘探提供必要的地质支撑。
- 分布规律台内滩碳酸盐岩台地古隆起嘉二段磨溪气田
Abstract: The oil and gas exploration for oolitic shoals in the Triassic platform margin in Sichuan Basin makes important breakthrough and headway. This has aroused the research interest for shoal body within wide carbonate platform. Taking the Bed A of the Jia2 Member in the Moxi Gas Field in central Sichuan Basin for an object of study, this article summarizes the development characteristics of the intraplatform shoal in the epicontinental carbonate platform, based on the analysis of the data of logging and coring in the region of interest. The intraplatform shoal is characterized by the shallowingupward sequence. A single shoal body is less than 4 meters in the thickness. Besides, the cumulative thickness and horizontal succession are both relatively inferior. The further research proves that the development and distribution of the oolitic shoals within the platform are controlled by the depositional palaeogeomorphology, water depth, turbulent of sea water and fluctuation of sea level. Meanwhile the research also indicates that the inherited palaeohigh within the epicontinental carbonate platform is benefit to develop the shoal vertically and horizontally. However, the palaeogeomorphologic differentiation causes horizontally great variation of intraplatform shoal. All of the investigation has laid a solid geologic foundation for the further exploration.
- distribution

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[1]	廖慧鸿, 苏中堂, 马慧, 孙珮婕. 滇东北地区晚奥陶世碳酸盐岩台地消亡的古环境因素 . 沉积学报, 2024, 42(2): 434-444. doi: 10.14027/j.issn.1000-0550.2023.094
[2]	丁一, 刘树根, 文龙, 文华国, 陈代钊, 宋金民, 王瀚, 王林康, 陈明思, 陈荣庆, 李智武. 中上扬子地区震旦纪灯影组沉积期碳酸盐岩台地古地理格局及有利储集相带分布规律 . 沉积学报, 2024, 42(3): 928-943. doi: 10.14027/j.issn.1000-0550.2023.135
[3]	苏成鹏, 李飞, 谭秀成, 王小芳, 龚峤林, 李明隆, 芦飞凡, 唐浩, 邓嘉婷, 李红. 古代碳酸盐岩台地自生泥质组分成因及意义 . 沉积学报, 2021, 39(3): 550-570. doi: 10.14027/j.issn.1000-0550.2020.072
[4]	任娜娜, 韩波, 张军涛, 冯菊芳, 王晓涛, 朱爽, 马强, 田海芹, 何治亮. 海水进退、滩坪出没、云化岩溶等与碳酸盐岩储层关系研究——以上扬子地台龙王庙组为例 . 沉积学报, 2018, 36(6): 1190-1205. doi: 10.14027/j.issn.1000-0550.2018.068
[5]	付坤荣, 黄理力, 祝怡, 冯翔艺蓝, 章巧, 关小丽, 高达. 塔中地区晚奥陶世碳酸盐台缘与台内沉积差异——定性和定量的碳酸盐岩微相综合分析 . 沉积学报, 2018, 36(1): 101-109. doi: 10.3969/j.issn.1000-0550.2018.012
[6]	黎荣, 胡忠贵, 张航, 胡明毅, 陈轩, 朱宜新, 刘菲. 川东卧龙河-洋渡溪区带长兴组台内礁滩沉积格局及有利储集体展布 . 沉积学报, 2016, 34(5): 973-982. doi: 10.14027/j.cnki.cjxb.2016.05.016
[7]	. 塔中地区良里塔格组台缘颗粒滩沉积特征及分布规律 . 沉积学报, 2014, 32(2): 354-364.
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磨溪气田嘉二段陆表海碳酸盐岩台地内滩体发育规律

谭秀成

西南石油大学资源与环境学院成都610500

通讯作者: 谭秀成

收稿日期: 1900-01-01
修回日期: 1900-01-01
刊出日期: 2009-10-10

关键词:

分布规律台内滩碳酸盐岩台地古隆起嘉二段磨溪气田

摘要: 近年来，四川盆地三叠系台缘鲕滩的油气勘探取得了重大的突破和进展，激发了人们对广阔台地内部滩体的研究兴趣。以四川盆地川中地区磨溪气田嘉二2A层为研究对象，通过对区内钻孔的测、录井及岩心芯资料的分析，总结了陆表海碳酸盐岩台地上台内滩体发育特征：向上变浅序列发育、单滩体厚度一般小于4 m、累积厚度较小以及横向连续性较差。进一步分析讨论后认为，沉积期古地貌、古水深、海水动荡程度以及古海平面相对升降变化共同控制了台内滩的发育与分布，结果表明陆表海碳酸盐岩台地内继承性古隆起是台内滩体的有利发育区，形成的台内滩体具有一定的厚度规模和较大分布面积，但是台地内部的隆坳地形分异使滩体横向分布变化较大。这些认识可为台内鲕滩储层的下一步勘探提供必要的地质支撑。

English Abstract

Shoal Development within the Epicontinental Carbonate Platform, Jia 2 Member, Lower Triassic, Moxi Gas Field, Central Sichuan Basin

TAN Xiucheng

.School of Resource and Environment, Southwest Petroleum University, Chengdu610500;

Corresponding author: TAN Xiucheng

Received Date: 1900-01-01
Rev Recd Date: 1900-01-01
Publish Date: 2009-10-10

Keywords:

distribution

Abstract: The oil and gas exploration for oolitic shoals in the Triassic platform margin in Sichuan Basin makes important breakthrough and headway. This has aroused the research interest for shoal body within wide carbonate platform. Taking the Bed A of the Jia2 Member in the Moxi Gas Field in central Sichuan Basin for an object of study, this article summarizes the development characteristics of the intraplatform shoal in the epicontinental carbonate platform, based on the analysis of the data of logging and coring in the region of interest. The intraplatform shoal is characterized by the shallowingupward sequence. A single shoal body is less than 4 meters in the thickness. Besides, the cumulative thickness and horizontal succession are both relatively inferior. The further research proves that the development and distribution of the oolitic shoals within the platform are controlled by the depositional palaeogeomorphology, water depth, turbulent of sea water and fluctuation of sea level. Meanwhile the research also indicates that the inherited palaeohigh within the epicontinental carbonate platform is benefit to develop the shoal vertically and horizontally. However, the palaeogeomorphologic differentiation causes horizontally great variation of intraplatform shoal. All of the investigation has laid a solid geologic foundation for the further exploration.

谭秀成. 磨溪气田嘉二段陆表海碳酸盐岩台地内滩体发育规律[J]. 沉积学报, 2009, 27(5): 995-1001.

引用本文:

谭秀成. 磨溪气田嘉二段陆表海碳酸盐岩台地内滩体发育规律[J]. 沉积学报, 2009, 27(5): 995-1001.

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磨溪气田嘉二段陆表海碳酸盐岩台地内滩体发育规律

通讯作者:
谭秀成

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Shoal Development within the Epicontinental Carbonate Platform, Jia 2 Member, Lower Triassic, Moxi Gas Field, Central Sichuan Basin

Corresponding author: TAN Xiucheng

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磨溪气田嘉二段陆表海碳酸盐岩台地内滩体发育规律

西南石油大学资源与环境学院成都610500

通讯作者: 谭秀成

English Abstract

Shoal Development within the Epicontinental Carbonate Platform, Jia 2 Member, Lower Triassic, Moxi Gas Field, Central Sichuan Basin

.School of Resource and Environment, Southwest Petroleum University, Chengdu610500;

Corresponding author: TAN Xiucheng

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磨溪气田嘉二段陆表海碳酸盐岩台地内滩体发育规律

通讯作者: 谭秀成

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Shoal Development within the Epicontinental Carbonate Platform, Jia 2 Member, Lower Triassic, Moxi Gas Field, Central Sichuan Basin

Corresponding author: TAN Xiucheng

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磨溪气田嘉二段陆表海碳酸盐岩台地内滩体发育规律

西南石油大学资源与环境学院成都610500

通讯作者: 谭秀成

English Abstract

Shoal Development within the Epicontinental Carbonate Platform, Jia 2 Member, Lower Triassic, Moxi Gas Field, Central Sichuan Basin

.School of Resource and Environment, Southwest Petroleum University, Chengdu610500;

Corresponding author: TAN Xiucheng

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