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翻訳と辞書　辞書検索 [ 開発暫定版 ] スポンサード リンク High Karst Unit ： ウィキペディア英語版 High Karst Unit The High Karst Unit (or High Karst Zone) is a tectonic unit in Slovenia, Croatia, Italy, Bosnia and Herzegovina, Kosovo, Serbia, Montenegro and Albania. The unit consists of a stratigraphic sequence that was deposited between the Upper Carboniferous and the Eocene. The deposition started with marine sediments during the Upper Cretaceous and Permian. During the Early Triassic shallow-marine cabonates and siliciclastics are a sign of shallow-marine conditions. In the Middle Triassic deep water conditions were reached.〔 During the Late Triassic the depositional environment became shallower again, and a carbonate platform developed. This continued till the Eocene, when flysch was deposited.〔 In the north the High Karst Unit is overthrust by Southern Alpine units. In the east the Pre-Karst Unit and the Bosnian Flysch overthrust it. The High Karst Unit overthrusts the Dalmatian Zone in the west and the Budva-Cukali Zone in the southwest. In the south the unit is cut off by the Skadar-Peć Fault and borders the Western Vardar Ophiolitic Unit.〔 The most prominent fault that runs through the High Karst Unit is the Split-Karlovac Fault.〔 ==References== 抄文引用元・出典: フリー百科事典『 ウィキペディア（Wikipedia）』 ■ウィキペディアで「High Karst Unit」の詳細全文を読む スポンサード リンク 翻訳と辞書 : 翻訳のためのインターネットリソース Copyright(C) kotoba.ne.jp 1997-2016. All Rights Reserved.