| 释义 |
siliciclastic 英sɪlaɪtʃɪk'læstɪk美sɪlaɪtʃɪk'læstɪk BNC⁸⁶⁶⁶⁰⁺⁹
基本例句
硅质碎屑的¹⁰⁰
Occurrence of both carbonate and siliciclastic sources, active hydrodynamic regimes, alternate dry and wet climates, and the fluctuation of sea level are main factors for forming mixed sediments.
形成混合沉积的条件是具备碳酸盐和硅质碎屑两类物源、活跃的水动力和干湿交替的气候，此外，海平面的相对波动也会造成积极的影响。 cnki
Sedimentogenic significance of mixed carbonate and siliciclastic sediments is emphasized.
对碳酸盐与陆源碎屑的混合沉积的研究具有重要意义。 cnki
Carboniferous siliciclastic rocks in Tazhong area, Tarim Basin are good reservoirs.
塔中地区石炭系碎屑岩是优质储层。 cnki
The basins contain18 to20 kilometers of pre Upper Permian carbonate and post Upper Permian siliciclastic sedimentary fill.
盆地包含18至20千米的二叠纪的碳酸岩和硅质碎屑沉积物。 www.resip.ac.cn |