Carbonate rocks can also be broken and reworked to form clastic sedimentary rocks. 此外，碳酸鹽巖也可被破碎并被改造成碎屑沉積巖。
The marine hydrocarbon source rock is generally carbonate rock of isolated platforms and interplatform troughs in the Baise basin. 摘要百色盆地海相烴源巖主要為孤立臺地和臺間海槽碳酸鹽巖。
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