The Tertiary stratum of Iran basin has thickly and broadly deposited great carbonate sediments.
伊朗盆地第三系地层沉积了巨厚的碳酸盐岩，且分布广泛。
Carbonate sediments in all environments are basically products of an ancient biochemical system.
一切环境的碳酸盐沉积物，基本上都是古代生物化学体系的产物。
This makes carbonate sediments on the floor of the ocean that are subducted back into the Earth though plate tectonics.
这样在海洋表面的碳酸盐的沉积物通过板块构造返回地球中。
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