Geochemical element balance during tropical weathering. Hercynian Rheinisches Schiefergebirge (Germany): a case study  

作　　者：Jean Thein Matthias Stoffels 

机构地区：[1]Geological Institute Bonn University,D-53115 Bonn,Germany

出　　处：《Journal of Geoscientific Research in Northeast Asia》2005年第1期48-52,共5页东北亚地学研究（英文版）

摘　　要：Introduction The Rheinisches Schiefergebirge, the northern,non metamorphic part of the Hercynian orogen in Middle Europe is one of the most excellent examples of a stable continental area, deeply weathered under a tropical to subtropical climate during upper Mesozoic and especially Paleogene periods.　　Introduction 　　The Rheinisches Schiefergebirge, the northern,non metamorphic part of the Hercynian orogen in Middle Europe is one of the most excellent examples of a stable continental area, deeply weathered under a tropical to subtropical climate during upper Mesozoic and especially Paleogene periods.

关 键 词：热带天气 地球化学元素 海西期 德国 

分 类 号：P595[天文地球—地球化学]