Geochemistry of carbonate cements of ODP Leg 112 samples

The evolution of pore fluids migrating through the forearc basins, continental massif, and accretionary prism of the Peru margin is recorded in the sequence of carbonate cements...孔隙流体在秘鲁陆缘（Peru margin）的弧前盆地（forearc basins）、大陆地块（continental massif）及增生楔（accretionary prism）中运移的演化过程，被记录于碳酸盐胶结物的序列当中。