斜坡沉积 meaning in Chinese
cinoform
clinoform
clinothem deposit
Examples
- Deep dissolution is the important diagenesis for forming pores because of its fast buried rate and good preservation of organic matter . the difference is that deep dissolution is strong and fills large amount of bitumen in the section of danzhai , which shows they are pores when the oil and gas assembled ; but pores are comparatively less in the section of sandu
由于斜坡沉积埋藏速度快，较快进入埋藏成岩环境，所以深溶作用有机溶解作用是该地区最主要的成孔成岩作用，所不同的是：丹寨剖面该种作用较强，而且孔内大部分灌入沥青，充分说明其是聚集期孔隙而三都剖面这种孔隙相对较少。 - Algae - rich carbonate of cambrian is typical sediment of foreslope facies in sandu and danzhai , eastern guizhou province . after sediment , it experiences many changes of diagenetic environment , and takes place much diagenetic altercation , among which the biggest is salt water dolomilization , and then is compaction , recrystallization , pressure solution , organic dissolution , burial dolomilization , cementation and silicification
贵州省东部三都丹寨地区中上寒武统富藻碳酸盐岩是典型的斜坡沉积,其在沉积后漫长的地质历史时期内，经受了诸多成岩环境的改造，发生了极大的成岩变化，最大的成岩变化为咸水云化，其他的成岩作用有压实作用重结晶作用压溶作用有机溶解作用埋藏云化作用胶结作用及硅化作用等。