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1)  kerogen-pyrolysis gas
源岩热解气
1.
A set of indexes for differentiating kerogen-pyrolysis gas and oil-cracked gas is presented based on geologic analysis and thermal simulation experiments on source rocks and crude oil samples from the Es4.
济阳坳陷民丰地区天然气存在源岩热解和原油裂解成因的争议,利用古近系沙四段烃源岩、原油样品的热模拟实验与地质分析相结合的方法,提出了源岩热解气和原油裂解气的鉴别标志。
2)  gas from the pyrolysis of source rock
烃源岩热解气
3)  Magma hot source
岩浆热源
4)  rock pyrolysis
岩石热解
1.
Application of rock pyrolysis analysis in Hailaer Basin;
岩石热解分析技术在海拉尔盆地的应用
2.
The Advantages of Rock Pyrolysis Logging Technology in Oil Gas Zone Evaluation;
岩石热解录井技术在油气层评价中的优势
3.
The quantitative interpretation and evaluation method for the gas chromatography of rock pyrolysis in lower permeability reservoir
低渗透率储集层岩石热解气相色谱量化解释评价方法
5)  shale purolysis
页岩热解
6)  gas source rocks
气源岩
1.
Geochemical characteristics of coalbed gas source rocks and analysis of gas potential in Qinshui Basin;
沁水盆地煤层气气源岩地球化学特征及气源潜力分析
2.
And whether the carbonate source rocks can be commercial oil source rocks and gas source rocks or not is an important problem, which concerns the direction of exploration and investment.
结果表明,车镇、沾化和东营凹陷下古生界碳酸盐岩均为非油源岩、非气源岩。
3.
The gas source rocks evolution are various in different formations and tectonic positions,the associated gas generation stage of up.
60℃/100m;不同层段、不同构造部位的气源岩演化具有明显的差异性,沙四上亚段气源岩现今开始大量生油和伴生气;沙四下亚段第一套气源岩主要生裂解气时期为馆陶组沉积末期至今;孔二段气源岩主要生裂解气时期为沙一沉积时期至今。
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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