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The Himalayan Geothermal Belt (HGB) is a region that extends for through India, Tibet, Yunnan, Myanmar and Thailand, and that contains many geothermal fields. ==Location== The Himalayan Geothermal Belt was formed as a result of the collision of the Indian Plate with the Eurasian Plate, which created the Himalayas. The belt is more than wide. The HGB has an extension to the westward that shows in warm or hot springs in the Peshawar region of Pakistan. These are clustered along the Main Karakoram Thrust, Main Mantle Thrust and Main Central Thrust. Some authors consider that the belt extends yet further west and should be called the Mediterranean-Himalayan Geothermal Belt. 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「Himalayan Geothermal Belt」の詳細全文を読む スポンサード リンク
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