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3. 黄海自生黄铁矿分布及同位素特征（据参考文献[
（a）黄海黄铁矿含量等值线平面分布图；（b）H-106孔黄铁矿硫同位素δ34S值；YSWC：黄海暖流；YSCC：黄海沿岸流
Fig.3. Distribution and isotopic characteristics of authigenic pyrite in the Yellow Sea (modified after references [31,54,55])
(a) Distribution of pyrite content in mud sediment of the Yellow Sea; (b) Sulfur isotopic compositions of core H-106 derived from the Yellow Sea.YSWC：Yellow Sea Warm Current；YSCC：Yellow Sea Coastal Current
