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亚洲内陆作为全球重要的风尘释放区，新生代以来，在全球气候变化和区域构造运动的双重影响下，亚洲内陆的环境格局发生了深刻的变化。保存在北太平洋的风尘沉积物记录了亚洲内陆风尘源区古环境演化的重要信息。前人普遍观点认为北太平洋地区风尘通量越高，指示亚洲风尘源区越干旱，然而也有观点指出风尘通量变化与源区干旱化程度并不是简单的线性关系。
Introduction to this Special Issue on Strata Formation on European Margins: A Tribute to EU-NA Cooperation in Marine Geology
European Margins Strata
2015/7/29
n the early fall of 1998, we sat gazing over the coastal ocean that surrounds Sicily. Scientists from around the world had gathered to participate in a SEPM-IAS (Society for Sedimentary Geology-Intern...