1) source-contacting gas reservoir
根缘气藏
1.
By combining the simulation study of hydrocarbon generation with the analysis of the periods of hydrocarbon accumulation,it is indicated that natural gas reservoirs in the studied area can be divided into two types:conventional trap gas reservoir and source-contacting gas reservoir.
结合生烃模拟研究及成藏期次的分析认为,研究区天然气藏分为2种类型,即常规圈闭气藏和根缘气藏,分别在中侏罗世晚期之前和早白垩世晚期之后成藏,主体上分别分布在以三眼井—泊尔江海子断裂为界的北部地区和南部地区。
2) source-contacting oil and gas
根缘油气藏(深盆油气藏)
3) source-contacting gas
根缘气
1.
Application of multi-level fuzzy judgment in source-contacting gas resource evaluation;
多层次模糊综合评判法在根缘气资源评价中的应用
2.
Experiments on the abnormal pressure of source-contacting gas (basin-centered gas) accumulation;
根缘气(深盆气)成藏异常压力属性实验分析
3.
Nonassociated gas can be classified as conventional gas accumulation with displacement migration,source-contacting gas accumulation with piston-type migration,and shale gas accumulation with the displacement and piston-type migrations.
游离相天然气主要包括置换式运移并聚集的常规储层气、活塞式运移并聚集的根缘气和兼具上述两种运移模式并具有复杂运聚机理的页岩气等,根据游离相天然气运聚的连续性动力平衡方程可以对不同运聚机理类型的天然气进行成藏描述。
4) deep basin gas (source-contacting gas accumulation)
深盆气(根缘气)
5) root edge
根缘(焊接),齿根缘
6) eastern Tibet
青藏东缘
1.
Study on petrology and mineral chemical compositions of deep-derived mafic enclaves from high-K igneous rocks in Liuhe-Xiangduo area, eastern Tibet showed that the enclaves belong to metamorphic rocks formed in the mid-lower crust.
对青藏东缘新生代六合 香多地区高钾岩系中镁铁质深源包体的岩石学和矿物化学成分的详细研究表明:六合 香多镁铁质深源包体为中 下地壳变质岩。
2.
The mineral assemblages of spinel-lherzolite xenoliths in Maguan Area, Eastern Tibet are Ol+Opx+Cpx+Spl.
青藏东缘马关尖晶石二辉橄榄岩包体的矿物组合为橄榄石 (Ol) +斜方辉石 (Opx) +单斜辉石 (Cpx) +尖晶石 (Spl)。
3.
Thermochronological studies suggest that two types of high-potassic magmatism occur in eastern Tibet and the time of igneous activities corresponds to 40-28 Ma and 16-0 Ma, respectively.
热年代学研究表明 ,青藏东缘存在两期新生代高钾岩浆活动 ,其活动时限分别为 40～ 2 8Ma和 16～ 0Ma。
补充资料：根缘
【根缘】
（术语）人之根性与境遇之缘务。玄义分记三曰：“根缘不同，就戒授五八十具等戒，就定教于观练薰修等定。”
（术语）人之根性与境遇之缘务。玄义分记三曰：“根缘不同，就戒授五八十具等戒，就定教于观练薰修等定。”
说明：补充资料仅用于学习参考，请勿用于其它任何用途。
参考词条