Carbonate rocks can also be broken and reworked to form clastic sedimentary rocks. 此外，碳酸盐岩也可被破碎并被改造成碎屑沉积岩。
The marine hydrocarbon source rock is generally carbonate rock of isolated platforms and interplatform troughs in the Baise basin. 摘要百色盆地海相烃源岩主要为孤立台地和台间海槽碳酸盐岩。
