1) non-reservoir sediment
非储集层沉积物
2) reservoir sedimentation
储集层沉积
1.
Two extreme modes of reservoir sedimentation: Active rift and passive rift;
储集层沉积的两种极端模式——主动裂谷和被动裂谷
3) reservoir sedimentary facies
储集层沉积相
4) reservoir sedimentation
储层沉积
1.
The reservoir sedimentation models are classified into rift model and sag model,which are fully represented in the passive rifts and active rifts,only different in sedimentary cycles that the active rift is bi-model with single cycle and the passive rift is bi-model with multi-cycle.
裂谷盆地的储层沉积模式主要分为断陷式和坳陷式,他们的沉积分异无论是在主动裂谷或是被动裂谷中都有充分体现,区别只在于沉积旋回上的差异,主动裂谷储层沉积为双模式单旋回;被动裂谷储层沉积为双模式多旋回。
5) nonreservoir
非储集层
6) reservoir sedimentology
储层沉积学
1.
Based on the fundamental principle of reservoir sedimentology, the formation mechanism of the braided river sandbodies in Zhangjiakou region is analyzed in this paper.
根据储层沉积学原理，对张家口地区辫状河砂体的成因进行分析，划分出３级层次界面和６种岩石相类型，对沉积、成岩作用与储层物性的关系进行了探讨。
2.
The study of reservoir sedimentology shows that the feldspar sandstone as a main type of sandstones developed in the central part of the Honggang region,Songliao Basin is characterized by low maturity,well to moderate sorting,moderate to poor roundness and low matrix contents.
对松辽盆地红岗地区中部含油组合的储层沉积学研究表明:研究区砂岩类型以长石砂岩为主,成熟度低,分选好-中等,磨圆中-差,杂基含量低;沉积构造类型多样,准同生变形构造十分发育;自西向东依次出现(扇)三角洲/浅湖、半深湖、深湖沉积,可划分为三种沉积体系,有利沉积相为(扇)三角洲前缘及浊积岩;成岩作用较弱,次生孔隙发育,属中孔中-低渗型储层。
补充资料：多层沉积层
分子式：
CAS号：
性质：由两种或两种以上相继沉积的金属构成的沉积层。这些沉积层可以由不同特性的同一金属或不同金属构成。如为了提高镍镀层的防护性，有时采用双层镍或三层镍镀层。又如为防护-装饰目的采用的铜/镍/铬三层镀层。
CAS号：
性质：由两种或两种以上相继沉积的金属构成的沉积层。这些沉积层可以由不同特性的同一金属或不同金属构成。如为了提高镍镀层的防护性，有时采用双层镍或三层镍镀层。又如为防护-装饰目的采用的铜/镍/铬三层镀层。
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