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1)  abyssal hearth
深层生烃热源
2)  deep source rocks
深层烃源岩
1.
In Tarim Basin,the deep source rocks,with depth deeper than four thousand meters,include the Cambrian and Ordovician marine carbonate rocks,the Triassic and Jurassic terrestrial mudstones,carbargillites and coals.
塔里木盆地深层烃源岩主要是指埋深大于4000 m的寒武—奥陶系海相碳酸盐岩和三叠—侏罗系陆相泥岩、碳质泥岩和煤。
3)  deep-seated hydrocarbon
深层烃
4)  source bed
烃源层
1.
An evaluation of the source bed in Upper Cretaceous Taizhou Formation,Subei basin;
苏北盆地上白垩统泰州组烃源层评价
5)  hydrocarbon source fault
烃源断层
6)  regenerated hydrocarbon source
再生烃源
1.
Based on analyses of accumulation material basement,event and mode in the east of Manjiaer region of the Tarim Basin,it has been found out that,besides kerogen source rocks rich in carbonate from Cambrian to Middle-Lower Ordovician,there also exist regenerated hydrocarbon source rocks represented by ancient reservoirs.
塔里木盆地满东地区的成藏物质基础、成藏事件和成藏模式分析表明,该地区除发育寒武系—中下奥陶统高有机质丰度的干酪根型烃源岩外,还发育以古油藏形式为主的"再生烃源",油气藏的形成可分为3个发展阶段:1)中加里东期的古隆起发育、古油气藏形成阶段;2)晚加里东期—印支期的古隆起隆升剥蚀、古油藏破坏并调整阶段;3)晚燕山期—喜山期的上构造层褶皱断裂发育、圈闭形成、以古油藏裂解气充注为主的阶段。
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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