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1)  active source rock
活跃烃源岩
1.
The active source rock distribution is studied in Bozhong Depression by analyzing the techniques of evolution history,basin simulation and geochemistry.
通过演化史分析、盆地模拟及地化分析技术对渤中坳陷活跃烃源岩的分布作了研究。
2)  hydrocarbon source rock
烃源岩
1.
Evaluation of geochemical characteristics of hydrocarbon source rock and gas-generating potential in Upper Tertiary, Baoshan Basin;
保山盆地上第三系烃源岩地化特征及气源潜力评价
2.
Distribution character and influential factor of hydrocarbon source rock of lower-Palaeozoic in the east of North China;
华北地区东部下古生界烃源岩特征及其影响因素
3.
Review on recovering method of organic matter abundance in hydrocarbon source rock;
烃源岩有机质丰度恢复方法综述
3)  Hydrocarbon source rocks
烃源岩
1.
Comparison and analysis of hydrocarbon source rocks in Yanchang and Yan′an Formations, Longdong Area;
陇东地区延长组、延安组烃源岩对比分析
2.
Using seismic and log information to predict and evaluate hydrocarbon source rocks: An example from rich oil depressions in Bohai Bay;
利用地震和测井信息预测和评价烃源岩——以渤海湾盆地富油凹陷为例
3.
Paleoclimatic information in stratigraphic records and its relation to the formation of hydrocarbon source rocks——A case study of the Paleogene strata in the Huanghekou subbasin of the Bohai Bay basin,China;
地层记录中的古气候信息及其与烃源岩发育的相关性——以渤海黄河口凹陷古近系为例
4)  source rock
烃源岩
1.
Study on "shallow maturation" of source rock in Jinhu Depression;
金湖凹陷烃源岩“浅熟”原因探讨
2.
Study on source rock features and resources evaluation of Yishu graben;
依舒地堑烃源岩及资源量评价
3.
Geochemistry of hydrocarbon source rocks in the Liupanshan basin at the northeastern margin of the Qinghai-Tibet Plateau;
青藏高原东北缘六盘山盆地烃源岩的地球化学特征
5)  source rocks
烃源岩
1.
Geochemical characteristics and source potential of the source rocks in Qingnan Subsag;
青南洼陷烃源岩地球化学特征及资源潜力
2.
Geochemical characteristics of source rocks in Yangxin Subsag;
阳信洼陷烃源岩地球化学特征
3.
Effect of igneous rocks on formation and evolution of source rocks in Yangxin Sag;
阳信洼陷火成岩对烃源岩形成及演化的作用
6)  low-evolutionary source rocks
化烃源岩
1.
Investigation of the thermal simulation of low-evolutionary source rocks bitumen "A" of the salt lacustrine facies in Qaidam Basin indicated that the range of temperature on the hydrocarbon generating fastigium in the thermal function are 200~270℃,and the source rocks are characterized by high relative abundance of the nonhydrocarbon and asphaltene.
柴达木盆地盐湖相低演化烃源岩沥青"A"的热模拟研究表明:在热作用下其排烃高峰在热模拟温度较低区间220~270℃,且以非烃和沥青质相对丰度最高为特征。
补充资料:烃源岩(见生石油天然气岩层)


烃源岩(见生石油天然气岩层)
source rock of oil and gas

  、~u以人‘峪iUU长天然气岩层01012丹nd即劝见生2
  
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