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Formation of Angerh Minue Cave in Asmari Karst Complex of Zagros Mountain, Iran

机译:伊朗扎格罗斯山Asmari岩溶群中Angerh ue穴的形成

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The Angerh Minue Cave, located in one km from west Angerh village which isabout 97 km far from Shiraz of Fars Province, the Cultural Capital of Iran. Themain entrance of the cave is at an altitude of 2430 having a depth of 176 m andlength 776 m. It developed along the bedding of limestone layers. AsmariFormation is the host rock of the Angerh Minue cave. Mountainous region ofZagros, where the Angerh Minue cave is located could be referred as seismicregion due to the presence of various basement faults, some of which are stillactive. In the present study, the geological process behind the formation ofAngerh Minue Cave has been tried toanalyze.
机译:Angerh Minue洞穴位于距Angerh西部村庄1公里的地方,该村庄距离伊朗文化之都Fars省Shiraz约97公里。洞穴的主要入口在海拔2430处,深度176 m,长度776 m。它沿着石灰岩层的地层发育。 AsmariFormation是Angerh Minue洞穴的宿主岩。 Angerh Minue洞穴所在的Zagros山区由于存在各种地下断层而被称为地震区,其中一些仍处于活动状态。在本研究中,尝试分析了安吉尔·米努埃(Angerh Minue)洞穴形成背后的地质过程。

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