2) organic facies
沉积有机相
1.
The Jurassic hydrocarbon source rocks on the north margin of Qaidam Basin could be divided into highstand marsh peat organic facies, forest marsh peat organic fades, shore-shallow lake organic facies and semideep-deep lake organic facies.
根据柴达木盆地北缘侏罗系烃源岩的有机岩石学、沉积学和有机地球化学特征将烃源岩的沉积有机相划分为４种类型，即高位泥炭沼泽有机相、森林泥炭沼泽有机相、滨浅湖有机相和半深湖－较深湖有机相。
2.
Directed by the theories such as Petroleum geology and Petroleum geochemistry,the source rocks of late cretaceous in Changling sag of southern Songliao basin are divided into organic facies A,organic facies B and organic facies B-C on the basis of the characteristics of organic petrology,sedimentology and organic geochemistry.
以石油地质学和石油地球化学为理论指导,通过对长岭凹陷上白垩统烃源岩的有机岩石学、沉积学和有机地球化学特征的综合分析,将沉积有机相划为3种类型,即有机相A、有机相B和有机相B-C。
3) sedimentary organic facies
沉积有机相
1.
According to the organic petrology,sedimentology and organic geochemistry of source rocks,the sedimentary organic facies in this area can be divided into three types:hemideep-deep lacustrine organic,shore-swamp organic and high-stand swamp organic facies.
根据其有机岩石学、沉积学和有机地球化学的特征,将该区沉积有机相划分为3种类型:高位沼泽有机相、滨浅湖-沼泽有机相和半深湖-深湖有机相。
2.
According to the characteristics of organic petrology, sedimentology and organic geochemistry, the source rocks of the Yanchang Formation in Zhenyuan - Jingchuan area in the south of Erdos basin are divided into three sedimentary organic facies including delta, coastal - shallow lake and semi - deep lake.
根据鄂尔多斯盆地南部镇原—泾川地区延长组烃源岩的有机岩石学、沉积学及有机地球化学特征将其划分为三种沉积有机相类型:三角洲有机相、滨浅湖有机相以及半深湖—较深湖有机相。
3.
Being synthetically analyzed with methods of organic geochemistry, organic and/or sedimentary petrology, the Xishanyao formation is divided into four sedimentary organic facies, which are high moor, forest swamp, running water swamp, and open water organic facies, with the running water swamp and forest swamp being the main facies of hydrocarbon forming.
以准噶尔盆地中侏罗统西山窑组为研究对象，通过有机岩石学、有机地球化学和沉积学的综合研究和分析，将西山窑组沉积期划分为四种沉积有机相：高位沼泽有机相，森林沼泽有机相，流水沼泽有机相和开阔水体。
4) depositional organic matter
沉积有机质
1.
The evolution features of depositional organic matters in orogenic belt may reflect a lot of geological information such as temperature, confining pressure, stress, strain, and so on.
介绍了沉积有机质演化的基本规律及其影响因素 。
5) Sedimentary organic matter
沉积有机质
1.
Micro-column chromatography for the separation of compound-grouped fractions of sedimentary organic matter;
一种适用于沉积有机质族组分分离的微型柱色谱法
2.
Source of sedimentary organic matter in the mud areas of the East China Sea shelf;
东海陆架泥质区沉积有机质的物源分析
3.
A method has been developed for the release and determination of biomarker compounds in the covalently bound biomarkers of higher evolution sedimentary organic matters by catalytic hydropyrolysis HYPY/GC-MS.
针对地质体中高演化沉积有机质,应用催化加氢热解/气相色谱-质谱方法测定了干酪根中以共价键结合的生物标志物。
6) lacustrine sediment
湖相沉积
1.
Carbon isotope composition of buried plant tissues in Ngoring shallow frozen lacustrine sediments;
鄂陵湖浅层冻结湖相沉积物中埋藏植物屑稳定碳同位素组成特征
补充资料：金属有机化合物化学气相沉积
分子式：
CAS号：
性质：用金属有机化合物热分解进行气相外延生长的方法。其基本原理是将含有外延材料组分的金属有机化合物气体通过载气输送到反应室，在一定温度下进行外延生长。MOCVD技术主要应用于III-V族II-VI族化合物半导体超晶格量子阱等低维材料生长和多元固溶体的多层异质结构材料的生长，还可用于制备高温超导薄膜，铁电薄膜，传感器薄膜，太阳能电池薄膜及其他金属薄膜。该技术工艺可控，操作简便及适用于大规模生产等优点。其缺点是所用源材料为易燃剧毒物质。
CAS号：
性质：用金属有机化合物热分解进行气相外延生长的方法。其基本原理是将含有外延材料组分的金属有机化合物气体通过载气输送到反应室，在一定温度下进行外延生长。MOCVD技术主要应用于III-V族II-VI族化合物半导体超晶格量子阱等低维材料生长和多元固溶体的多层异质结构材料的生长，还可用于制备高温超导薄膜，铁电薄膜，传感器薄膜，太阳能电池薄膜及其他金属薄膜。该技术工艺可控，操作简便及适用于大规模生产等优点。其缺点是所用源材料为易燃剧毒物质。
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