Development Controlling Factors and Forming Model for Source Rock of Yueguifeng Formation in Lishui-Jiaojiang Sag, the East China Sea Continental Shelf Basin
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摘要: 下古新统月桂峰组是东海陆架盆地丽水-椒江富生烃凹陷的主力烃源岩系.利用钻井、地震及烃源岩有机地球化学、古生物等资料，在烃源岩特征及其发育的构造-沉积与古气候背景分析的基础上，探讨了控制丽水-椒江凹陷下古新统月桂峰组烃源岩发育的主要因素，并建立了相应的形成模式.丽水-椒江凹陷月桂峰组烃源岩分布广、厚度大，存在多个厚度中心；有机质丰度较高，有机质类型以Ⅱ2型为主，处于成熟-高成熟阶段.月桂峰组烃源岩发育于分割性较强、相对封闭的湖泊环境和半湿润-湿润南亚热带型气候条件，以低等水生生物贡献为主.月桂峰组烃源岩的发育主要受沉积-沉降速率、母质来源及有机质保存条件等因素控制，其形成模式可概括为“快速沉降，湿润气候，水生有机质贡献为主，淡水-微咸水，弱氧化-弱还原环境”.Abstract: Source rock in Yueguifeng Formation of Lower Paleocene is the main source rock series in Lishui-Jiaojiang hydrocarbon generating sag of the East China Sea shelf basin. Using drilling, seismic data combined with organic geochemistry and paleontology data of hydrocarbon source rock, the development controlling factors for the Yueguifeng Formation of Lower Paleocene are discussed and the forming model also is established based on the analysis of characteristics of the hydrocarbon source rock and tectonic-sedimentary-paleoclimate development background in this study. It is found that source rocks in Yueguifeng Formation of Lishui-Jiaojiang sag are characterized by wide distribution, large thickness and multiple thickness centers abundance of organic matter, type Ⅱ2 dominated organic matter, and relatively high maturity. Development background of Yueguifeng Formation is an intensive separation and relatively closed lake environment with subhumid-humid subtropical climate condition, and predominantly aquatic organic matter contribution. Development of hydrocarbon source rocks in Yueguifeng Formation is mainly affected by deposit-sedimentation rate, parent material source and preservation condition of organic matter, and it could be concluded that its forming model features with "rapid subsidence, humid climate, aquatic organic matter contribution, fresh-brackish water, and weak oxidation-reduction environment".
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Key words:
- Yueguifeng Formation /
- source rock /
- controlling factor /
- forming model /
- Lishui-Jiaojiang sag /
- sediments
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图 1 丽水-椒江凹陷位置及构造单元划分
Fig. 1. Position and division of tectonic units of Lishui-Jiaojiang sag
图 2 月桂峰组烃源岩有机质类型(a)和丰度判别(b)
Fig. 2. Organic matter type and abundance for source rock of Yueguifeng Formation
图 3 WZ4-1-1井沉积与地球化学综合分析
Fig. 3. integrated sedimentary and geochemical section of WZ4-1-1 well
图 4 丽水-椒江凹陷月桂峰组沉积时期基底沉降速率直方图
Fig. 4. Subsidence rate of basement during the sedimentary period of Yueguifeng Formation in Lishui-Jiaojiang sag
图 5 WZ26-1-1井孢粉组合特征及古气候意义
Fig. 5. Characteristics of pollen assemblage of WZ26-1-1 well and its paleoclimatic significance
图 6 丽水-椒江凹陷沉积-沉降速率分布
Fig. 6. Spatial-temporal characteristics of subsidence rate of Lishui-Jiaojiang sag
图 7 月桂峰组烃源岩TOC与三环萜烷比值交汇图
Fig. 7. Intersection of the TOC and tricyclic terpane ratio in Yueguifeng Formation
图 8 月桂峰组烃源岩氧化-还原环境判别
Fig. 8. Discrimination of oxidation-reduction environment of Yueguifeng Formation
图 9 WZ4-1-1井月桂峰组烃源岩藻类含量和无定形含量交汇图
Fig. 9. Intersection of algae content with the amorphous content from Yueguifeng Formation of WZ4-1-1 well
图 10 丽水-椒江凹陷微量元素(Sr/Ba)与井深关系
Fig. 10. Trace elements (Sr/Ba) with well depth relation in Lishui-Jiaojiang sag
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