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中国科学院南京地质古生物研究所机构知识库
KMS Nanjing Institute of Geology and Palaeonotology,CAS
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中国科学院南京地质古... [1]
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Xiang Lei [1]
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2014 [1]
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科学通报 [1]
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埃迪卡拉纪-寒武纪过渡时期下扬子深水盆地氧化还原性质:来自浙西底本剖面铁组分及有机碳同位素的约束
期刊论文
科学通报, 2014, 卷号: 59, 期号: 23, 页码: 2278-2289
Authors:
袁余洋
;
蔡春芳
;
汪天凯
;
向雷
;
贾连奇
;
陈妍
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Submit date：2014/10/11
底本剖面
扬子地台
埃迪卡拉纪-寒武纪
铁组分
氧化还原
