“碳酸盐”造句

实质上裂缝可割切大多数类型的碳酸盐组织.
Essentially fractures can cut most types of carbonate fabric.

岩石的外表呈现交织的石英及碳酸盐细脉组成的网格构造.
Rock faces commonly show a stockwork of intersecting quartz and carbonate veins.

海绿石 、 碳酸盐骨骸碎屑 、 海相化石和胶磷矿普遍出现.
Glauconite, detrital carbonate skeletal debris, marine fossils, and collophane are commonly present.

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