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Lithostratigraphy and Microbiostratigraphy of Gadvan and Darian Formations in South Semirom, East of Zagros Basin, South-Central Iran

机译:伊朗中南部扎格罗斯盆地以东的南塞米隆姆Gadvan和Darian地层的岩石地层学和显微生物地层学

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This research focuses on the lithostratigraphy and microbiostratigraphy implications of the Gadvan and Darian Formations in a part of Zagros sedimentary basin. The Gadvan and Darian Formations in the study area with a thick-ness of 520 meters consist of gray to green marls and shales, dark-grey limestones and Orbitolina limestone with Late Barremian-Aptian age. According to the lithostratigraphic investigations, the Gadvan and Darian Formations in the study area are subdivided into eleven units. The upper boundary of the Darian Formation with the Kazhdomi Formation and the lower boundary of Gadvan Formation with the Fahliyan Formation are in the form of disconformity. Micropaleontological study of the Gadvan and Dariyan Formations has led to the recognition 20 families, 45 genera, 35 species of benthic foraminifera, 2 genera of pelagic foraminifera and 8 genera and species of the calcareous algae. In this research, three biozones have been recognized by distribution of the larger benthic foraminifera in the Gadvan and Dariyan Formations of the South Semirom, including: 1) Palorbitolina lenticularis-Choffatella decipiens Concurrent Range Zone (middle Late Barremian to early Early Aptian); 2) Praeorbitolina cormyi-Orbitolina (Mesorbitolina) lotzei Assemblage Zone (late Early Aptian); 3): Orbitolina (Mesorbitolina) texanae-Orbitolina (Mesorbitolina) parva Assemblage Zone (Middle to Late Aptian). Based on the identified foraminifera, the age of the Gadvan and Darian Formations in the study area is assigned to Late Barremian to Aptian.
机译:这项研究的重点是Zagros沉积盆地一部分的Gadvan和Darian地层的岩石地层学和微生物地层学意义。研究区的加德旺和达里安组厚度为520米,由灰至绿的泥灰岩和页岩,深灰色的石灰岩和具巴里米亚-阿普特时代晚期的Orbitolina石灰岩组成。根据岩石地层学调查,研究区域的加德文和达里安组被细分为11个单元。 Darian组与Kazhdomi组的上边界和Gadvan组与Fahliyan组的下边界呈不整合形式。对Gadvan和Dariyan组的微古生物学研究导致人们认识到20个科,45属,35种底栖有孔虫,2种上层有孔虫和8属钙质藻类。在这项研究中,三个较大的底栖有孔虫分布在南塞米隆姆南部的加德旺和达里扬组中,已识别出三个生物带,其中包括:1)缓坡小孢子-小球藻同时期分布带(巴雷米亚中晚期至阿普提安早期); 2)早熟斑节菜-早熟斑节集区(Mesorbitolina)lotzei 3):眶天牛(Mesorbitolina)德克萨斯州-眶天牛(Mesorbitolina)矮树丛聚集区(中至晚Aptian)。根据确定的有孔虫,将研究区的加德文和达里安组的年龄分配给巴里米亚晚期至阿普提安。

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