(Table T1) Cation exchange capacities and contribution of cations to CEC in s...

Fluid circulation at midocean ridge flank areas where the igneous crust is young and still hot and sediment cover is usually thin actually produces a major chemical exchange...在洋中脊侧翼区域（midocean ridge flank areas）中，火成地壳（igneous crust）尚年轻且仍处于高温状态，沉积物盖层（sediment cover）通常较薄，此处的流体循环实际上催生了大规模的化学交换过程……