原文服务方: 地球化学学报(英文)       
摘要:
The outcrop samples of the Tak Fa Formation (Lower Permian) in Phetchabun Province have been studied to determine their organic geochemical characteristic, depositional paleoenvironment, and hydrocarbon generation potential. The total organic carbon (TOC) values ranging from 1.42 to 4.58 wt% and extractable organic matter values ranging from 76.84 to 197.65 ppm of the Tak Fa Formation were generally low and associated with low S2 values (0.00–0.50 mg HC/g rock) and hydrogen index values in range of 0–32 mg/g TOC, although this could reflect highly thermal maturity and complex tectonic history. Thus, kerogen classification can be based on a nonbiomarker study for these outcrop samples instead. The non-biomarker plot, Pr/n-C17 and Ph/n-C18 from this study indicates that organic matter originally comes from type Ⅱ/Ⅲ kerogen. The samples were also investigated and indicated that the organic matter inputs were derived from mixed marine and terrigenous sources and deposited under suboxic to oxic conditions. The depositional environment of the Tak Fa Formation in this study is interpreted to be an estuarine environment or restricted lagoonal carbonate platforms. This has been achieved from normal alkane and isoprenoids distributions, terpane, and sterane biomarkers. Thus, the Tak Fa Formation is considered to be a hydrocarbon source rock during the time of the deposition. Although the geochemical data in this study indicate that the Tak Fa Formation has experienced high maturation, one or more locations could meet a condition that places this formation to be an active source rock. The approach and concepts presented in this study can be applied to similar evaporite-carbonate deposits in Thailand to find more petroleum plays.
推荐文章
Geological significance of nickeliferous minerals in the Fule Pb–Zn deposit, Yunnan Province, China
Nickeliferous
Permian Emeishan basalt
Fule Pb–Zn deposit
MVT deposit
Barrier layer
The effects of clay minerals and organic matter on nanoscale pores in Lower Paleozoic shale gas rese
Nanoscale pore
Clay minerals
Organic matter
OM–clay composites
Pore distribution characteristics
Pore connectivity
A preliminary study on ore-forming environments of Xianglushan-type iron deposit and the weathering
Emeishan basalt paleo-weathering crust
Xianglushan-type iron deposit
Ore-forming environment
Weathering mineralization
Western Guizhou Province
内容分析
关键词云
关键词热度
相关文献总数  
(/次)
(/年)
文献信息
篇名 Organic geochemistry of the Lower Permian Tak Fa Formation in Phetchabun Province, Thailand: implica
来源期刊 学科 地球科学
关键词 Biomarker Depositional environment Source inputs Tak Fa Formation Khao Khwang Platform
年,卷(期) 2022,(3) 所属期刊栏目
研究方向 页码范围 291-306
页数 15页 分类号
字数 语种 英文
DOI 10.1007/s11631-019-00370-w
五维指标
传播情况
(/次)
(/年)
引文网络
引文网络
二级参考文献  (0)
共引文献  (0)
参考文献  (0)
节点文献
引证文献  (0)
同被引文献  (0)
二级引证文献  (0)
2022(0)
  • 参考文献(0)
  • 二级参考文献(0)
  • 引证文献(0)
  • 二级引证文献(0)
研究主题发展历程
节点文献
Biomarker
Depositional environment
Source inputs
Tak Fa Formation
Khao Khwang Platform
研究起点
研究来源
研究分支
研究去脉
引文网络交叉学科
相关学者/机构
期刊影响力
地球化学学报(英文)
双月刊
2096-0956
52-1161/p
16开
贵阳市林城西路99号
1982-01-01
英语
出版文献量(篇)
230
总下载数(次)
0
总被引数(次)
0
论文1v1指导