翻訳と辞書 |
Geology of Azerbaijan : ウィキペディア英語版 | Geology of Azerbaijan
The Geology of Azerbaijan forms a constituent geological part of the Alpine fold belt. Sedimentary deposits embracing the southwestern parts of the Major and Minor Caucasus, including the intermountain Kur River trough, as well as the Mid- and South Caspian basins consist of diversity fold systems. The Earth's crust thickness in Azerbaijan varies in the range from 38 to 55 km. Its maximum thickness is observed in the Minor Caucasus area, while its minimum thickness is typical for the Talysh foothills. Geological setting of the area consists of sedimentary, volcanic-sedimentary, volcanic and terrestrial deposits embracing almost entire stratigraphic range beginning from Pre-Cambrian through Holocene time. ==Minerals== Azerbaijan is rich of fuel ore and non-ore minerals. Ore and non-ore minerals are spread mostly in mountainous territories (Small and Great Caucasus), fossil fuels in plain territories and South Caspian basin. In its turn, it caused development of ore industry in west and oil-gas industry in east.
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「Geology of Azerbaijan」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.
|
|