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2. 黄、东海泥质区（黄色部分）分布与洋流情况（据参考文献[
YDW：长江冲淡水；ZMCC：浙闽沿岸流；YSWC：黄海暖流；YSCC：黄海沿岸流；YSMW：黄海混合水；TWC：对马暖流；TWWC：台湾暖流；KC：黑潮
Fig.2. Distribution of mud sediment (yellow) and ocean current system of the Yellow Sea and the East China Sea (modified after references [32,33])
YDW: Yangtze River Diluted Water; ZMCC: Zhe-Min Coastal Current; YSWC: Yellow Sea Warm Current;YSCC: Yellow Sea Coastal Current; YSMW: Yellow Sea Mixing Water; TWC: Tsushima Warm Current;TWWC: Taiwan Warm Current; KC: Kuroshio Current
