阿拉伯板块东北部的构造发展——以伊拉克北部库尔德斯坦地区的Pirmam和Bana-Bawi背斜为例

Ala A. Ghafur , Varoujan K. Sissakian , Nadhir Al-Ansari , Hassan O. Omer , Hawkar A. Abdulhaq
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引用次数: 1

摘要

Pirmam和Bana-Bawi背斜是两个细长的背斜,位于伊拉克北部库尔德斯坦地区(KRI)的中北部,阿拉伯板块的东北部。除了估计一些冲积扇和河流阶地的沉积和切割速率外,我们还使用卫星图像和地质图来解释所提供的数据,并计算向上和向下(沉降)的速率。大多数已取得的数据都是在实地核查的。Pirmam背斜的抬升和沉降速率分别为8.613 mm/100年和7.962 mm/100年,而Bana-Bawi背斜的抬升率分别为3.036 mm/100年或4.365 mm/100年。横向生长的迹象是存在水隙、风隙、梯队俯冲、鲸背形状和不同类型的山谷。我们计算了科里河和巴斯托拉河的沉积速率和切割速率。前者分别为5.204毫米/100年和5.555毫米/100年,而后者分别为3.469毫米/100年、8.731毫米/100年。此外,我们还计算了新旧冲积扇的沉积速率和切割速率。前者分别为1.665毫米/100年和0.722毫米/100年,而后者分别为3.036和4.365毫米/100岁。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Tectonic development of northeastern part of the Arabian Plate: Examples from Pirmam and Bana Bawi anticlines in the Kurdistan region of north Iraq

The Pirmam and Bana Bawi anticlines are two elongated anticlines located in the central northern part of the Kurdistan Region of north Iraq (KRI), in the northeastern part of the Arabian Plate. We have used satellite images and geological maps to interpret the presented data and to calculate the rates of uplift and down wards (subsidence) amounts, besides estimating the rates of deposition and incision of some alluvial fans and stream terraces. Most of the achieved data were checked in the field. In the Pirmam anticline the rate of the uplift and subsidence is 8.613 mm/ 100 year and 7.962 mm/ 100 year, respectively, whereas in the Bana Bawi anticline the rates are 3.036 mm/ 100 year and 4.365 mm/100 year, respectively. The indications of the lateral growth are the presence of water gaps, wind gaps, en-echelon plunging, whale-back shape and different types of valleys. We have calculated the depositional and incision rates in the Kori and Bastoora streams. They are 5.204 mm/ 100 year and 5.555 mm/ 100 year, respectively in the former, whereas in the latter are 3.469 mm/100 year and 8.731 mm/ 100 year, respectively. Moreover, we have calculated the depositional and incision rates in old and recent alluvial fans. In the former, they are 1.665 mm/ 100 year and 0.722 mm/ 100 year, respectively, whereas in the latter are 3.036 and 4.365 mm/ 100 years, respectively.

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