黄、东海陆架泥质区自生黄铁矿成因及其控制因素
常鑫1(
),张明宇1,谷玉1,王厚杰1,2,刘喜停1,2()
),张明宇1,谷玉1,王厚杰1,2,刘喜停1,2()
Formation Mechanism and Controlling Factors of Authigenic Pyrite in Mud Sediments on the Shelf of the Yellow Sea and the East China Sea
Xin Chang1(),Mingyu Zhang1,Yu Gu1,Houjie Wang1,2,Xiting Liu1,2()
),Mingyu Zhang1,Yu Gu1,Houjie Wang1,2,Xiting Liu1,2()
图7. 东海陆架沉积物硫酸盐还原速率和黄铁矿硫埋藏速率与有机碳埋藏速率之间的关系［
Fig.7. The linear relationship between sulfate reduction rate,pyrite sulfur burial rate and organic carbon burial rate in the East China Sea continental shelf sediments[
