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Considering Changes in Thickness of Hambast Formation Deposits in Different Section of Central Iran

机译:考虑伊朗中部不同地区的汉堡包形成层厚度变化

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Lithostratigraphy studies on Hambast Formation deposits in Shorjestan section indicate that in this section, Hambast Formation with 23 m thickness has 2 units (6 and 7). The 6th unit includes 6.5 m marly limestone and red, green and gray shale layers and the 7th unit includes 16.5 m red to purple limestone besides red and gray shale. A comparison between under studied section with 4 other sections in Abadeh and Shahreza indicates that regarding probable reasons such as different procedures of tectonic activities in floor of sedimentary basin, differentiation in sedimentation rate and different depths in sedimentary basin, thickness and lithology of these deposits are different with each other in a way that in Esfeh section in Shahreza region, deposits of Shahreza informal formation have more thickness and different lithology in comparison with Abadeh and Shorjestan sections.
机译:Shorjestan断面中的Hambast组沉积物的岩石地层学研究表明,该段中厚23 m的Hambast组有2个单元(6和7)。第6个单元包括6.5 m的灰白色石灰岩以及红色,绿色和灰色的页岩层,第7个单元除了红色和灰色的页岩之外还包括16.5 m的红色至紫色石灰岩。将正在研究的部分与Abadeh和Shahreza中的其他4个部分进行比较表明,考虑到可能的原因,例如沉积盆地底部的构造活动的程序不同,沉积速率的差异以及沉积盆地的深度不同,这些沉积物的厚度和岩性是彼此之间的不同之处在于,在Shahreza地区的Esfeh剖面中,与Abadeh和Shorjestan剖面相比,Shahreza非正式构造的沉积物具有更大的厚度和不同的岩性。

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