伊朗西南部扎格罗斯盆地上二叠统大兰组微生物地层学与岩石地层学

Pedram Rafiee, D. Baghbani, A. Aghanabati, M. Arian
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引用次数: 2

摘要

本研究的目的是对扎格罗斯盆地上二叠统大兰组(1井)进行微生物地层学和岩石地层学研究。伊朗西南部上二叠统大兰组含大量天然气,由三段组成:下大兰段对应于Wordian—Capitanian;北段为最新的capitian期,上大兰段对应于吴家坪期至长兴期。下、上大兰段主要为灰岩、白云质灰岩,纳尔段主要为硬石膏和薄白云岩夹层。生物地层学的研究使得从世界纪到长兴纪(中晚二叠世)的有孔虫个体化成为可能。根据具有重要地层意义的动物和植物的地层分布,提出了上二叠统大兰组的7个生物带和年龄的确定:7 .长兴地区副副valvulinoides septulifera带4 .长兴期(长兴期)直肠托毛区(五甲平间)沙尼塔区(Capitanian)副瓣带(capitian)球瓣带(世界语)Eoverbeekina区(世界)
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Micro Biostratigraphy and Lithostratigraphy of the Upper Permian Dalan Formation (Zagros Basin, Southwest Iran)
The objective of the present study is to perform Microbiostratigraphy and Lithostratigraphy of the Upper Permian Dalan Formation at a Well (Well 1) in the Zagros Basin. The Upper Permian Dalan Formation contains vast gas reservoirs in the southwest Iran and is composed of three Members: The Lower Dalan Member corresponds to Wordian to Capitanian; the Nar Member is latest Capitanian and the Upper Dalan Member corresponds to Wuchiapingian to Changhsingian. Lower and Upper Dalan Members include mainly limestone, dolomitic limestone and Nar member mostly consists of anhydrite and thin interlayer of dolomite. The biostratigraphic study allows individualizing Foraminifers from the Wordian to the Changhsingian (Middle to Late Permian). Based on the stratigraphic distributions of the Biostratigraphically significant fauna and flora the following 7 biozones and age determinations are proposed in the Upper Permian Dalan Formation: 7. Paraglobivalvulinoides septulifera zone (Changhsingian) 6. Paradagmarita zone (Changhsingian) 5. Rectostipulina zone (Wuchiapingian) 4. Shanita zone (Capitanian) 3. Paraglobivalvulina zone (Capitanian) 2. Globivalvulina zone (Wordian) 1. Eoverbeekina zone (Wordian)
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