| 南海南沙海域沉积盆地构造演化与油气成藏规律 |
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| 引用本文： | 杨明慧,张厚和,廖宗宝,罗晓华,雷志斌,张少华,张雨田,李毅玮.南海南沙海域沉积盆地构造演化与油气成藏规律[J].大地构造与成矿学,2017,41(4):710-720. |
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| 作者姓名： | 杨明慧 张厚和 廖宗宝 罗晓华 雷志斌 张少华 张雨田 李毅玮 |
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| 作者单位： | 1. 中国石油大学(北京)油气资源与探测国家重点实验室,北京 102200;中国石油大学(北京)地球科学学院,北京 102200;2. 中海油研究总院,北京,100028;3. 中国冶金地质总局第二地质勘查院,福建福州,350108;4. 中国石油大学(北京)地球科学学院,北京,102200;5. 西北大学大陆动力学国家重点实验室,陕西西安,710069 |
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| 基金项目： | 国家科技重大专项，大陆动力学国家重点实验室基金 |
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| 摘 要： | 据钻井、地震剖面、区域地质及磁异常条带分析解释,南沙海域及其邻区的主要沉积盆地的形成演化受裂谷起始不整合面和破裂不整合面分隔,可分为前裂谷期、裂谷期和后裂谷期3个构造阶段。大中型油气藏相关数据的统计表明,南沙海域及邻区大中型油气藏的成藏要素和油气田发育受构造阶段控制。(1)烃源岩发育具有分期、分区特征,礼乐盆地发育前裂谷期、裂谷1幕烃源岩;万安、曾母、西北巴拉望盆地发育裂谷2幕烃源岩,文莱-沙巴盆地发育后裂谷期烃源岩。(2)储层发育具有分期、分带特征,表现为外带老(裂谷2幕)、内带新(后裂谷期)。(3)圈闭类型包括构造、岩性地层圈闭及构造-岩性地层等因素形成的复合圈闭,大致具有内带以地层圈闭为主,外带以构造圈闭为主的特征。(4)大中型油气田分布具有外带砂岩富油气、内带碳酸盐岩富气特点。(5)南沙海域及邻区发育两个后裂谷期主含油气区,即东部巴兰三角洲砂岩背斜油气区和西部卢卡尼亚碳酸盐台地气区。其中,大中型气田的成藏要素组合为裂谷2幕烃源岩、后裂谷期碳酸盐岩储层和地层圈闭;大中型油气田则为后裂谷期烃源岩、砂岩储层和背斜圈闭。
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| 关 键 词： | 构造阶段 油气聚集 南沙海域 南海 |
Tectonic Evolution and Hydrocarbon Accumulation of the Sedimentary Basins in Nansha Sea Waters (South China Sea) |
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| YANG Minghui,ZHANG Houhe,LIAO Zongbao,LUO Xiaohua,LEI Zhibin,ZHANG Shaohua,ZHANG Yutian,LI Yiwei.Tectonic Evolution and Hydrocarbon Accumulation of the Sedimentary Basins in Nansha Sea Waters (South China Sea)[J].Geotectonica et Metallogenia,2017,41(4):710-720. |
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| Authors: | YANG Minghui ZHANG Houhe LIAO Zongbao LUO Xiaohua LEI Zhibin ZHANG Shaohua ZHANG Yutian LI Yiwei |
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| Abstract: | The tectonic stages of major sedimentary basins in the Nansha sea waters and its adjacent region (South China Sea) can be divided into pre-rift, syn-rift and post-rift stages by rift-onset unconformity and break-up unconformity based on a synthetic analysis of drilling data, seismic profiles, regional geology and magnetic anomalies. Moreover, from a view of hydrocarbon exploration, the reservoir-forming factors of the large and middle size hydrocarbon fields in this area are influenced by the tectonic stages, and the reasons are as follows: (1) The source rocks within different domains developed in different tectonic stages, more specifically, the source rocks within Reed Bank Basin mainly developed in pre-rift stage (the Early Cretaceous) and the 1st period of syn-rift stage (Paleocene to Eocene), the source rocks within Nam Con Son Basin, Zengmu Basin and Northwest Palawan Basin mainly developed in the 2nd period of syn-rift stage (the Late Oligocene to Early Miocene), while the source rocks within Brunei?Sabah Basin mainly developed in the post-rift stage (the Middle?Late Miocene); (2)The reservoir rocks within different zones also developed in different tectonic stages, generally speaking, the reservoir rocks within the outer zone (Balingian Province and the offshore area of Nam Con Son Basin developed Lower Miocene and Oligocene to Lower Miocene sandstone reservoirs, respectively; and Northwest Palawan Basin developed the Upper Oligocene to Lower Miocene carbonate reservoirs) are usually older than these within the inner zone (the Middle?Upper Miocene reservoirs mainly consist of sandstones within Brunei?Sabah Basin and carbonate rocks within Nam Con Son Basin and Zengmu Basin); (3)Trap styles in this area mainly include structural, lithologic, stratigraphic and composite traps, and the inner zone mainly developed stratigraphic traps, while the outer zone usually developed structural traps; (4) In terms of the distribution of large and middle size hydrocarbon fields, the sandstone reservoirs within the outer zone mainly accumulated oil and gas, while the carbonate reservoirs usually formed gas fields; and (5) There are two hydrocarbon-rich domains in the Nansha sea waters and its adjacent region, which are the oil- and gas-rich domain in the East (the offshore of Brunei?Sabah) and the gas-rich domain in the West (the offshore of West Sarawak). Furthermore, the reservoir-forming factors of the large and middle size gas fields are the Upper Oligocene to Lower Miocene source rocks, the Middle to Upper Miocene carbonate reservoirs and stratigraphic traps, while the reservoir-forming factors of the large and middle size oil and gas fields are the Middle to Upper Miocene source rocks, sandstone reservoirs and structural traps. |
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| Keywords: | tectonic evolution hydrocarbon accumulation Nansha sea waters South China Sea |
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