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Jebel Sasan ((アラビア語:جبل ساسان,چياى ساسان)) is a large hill in the Tel Afar District of Nineveh Province of northern Iraq. The name may also be rendered as Jabal Sasan. ==Geology== Jebel Sasan is in a transitional folded zone between an alpinotype area to the northeast and the Arabian Shield to the southwest. Tectonic movements in the Late Cretaceous caused formation of a rapidly subsiding trough aligned east-west passing below Jabal Sinjar and Jabal Sasan into the Butmah area. Open-sea globigerina sedimentation filled the trough at about the same rate as subsidence throughout the Late Cretaceous. The crystalline basement in the Jebel Sasan area is at a depth of about . 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「Jebel Sasan」の詳細全文を読む スポンサード リンク
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