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1)  benthal deposit
水底有机沉积
2)  subaqueous deposit
水底沉积
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3)  benthic deposit
水底沉积物
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 。
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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。
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6)  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。
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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。

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