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4. 杭州湾YS6钻孔孔隙水剖面（据参考文献[
阴影部分指示SMTZ、硫酸盐还原生成硫化带，钻孔位置见图6
Fig.4. Porewater profile of core YS6 from the Hangzhou Bay (modified after reference [
The shaded part indicates the SMTZ,where sulfide zone is formed by sulfate reduction. The core location is presented in Fig. 6
