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Deep seismic reflection study over the Vindhyans of Rajasthan: Implications for geophysical setting of the basin

机译:拉贾斯坦邦Vindhyans的深层地震反射研究:对盆地地球物理环境的启示

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This paper presents results of high-resolution deep seismic re???ection pro???ling of the Proterozoic Vindhyan basin of the Rajasthan area along the Chandli a€“Bundi a€“Kota a€“Kunjer pro ???le.Seismic images have been used to estimate the thickness of Vindhyan strata as well as to understand the tectonic framework of the basin.The results are constrained by gravity,magnetic and magne-totelluric data.The study reveals gentle SE-dipping re???ection bands representing the Vindhyan strata.The seismic sections depict gradual thickening of the Vindhyan succession towards south-east from Bundi.The velocities of the upper and lower Vindhyans are identi???ed as 4.6 a€“4.8 km/s and 5.1 a€“5.3 km/s.The NW limit of the Vindhyan basin is demarcated by the Great Boundary Fault (GBF)that manifests as a 30 km wide NW dipping thrust fault extending to a depth of 30 km.
机译:本文介绍了沿Chandli-Bundi a-Kota a-Kunjer pro-le沿拉贾斯坦邦地区的元古代Vindhyan盆地进行高分辨率深地震反射剖面分析的结果。地震图像已被用于估算Vindhyan地层的厚度以及了解盆地的构造框架。结果受到重力,磁和镁-大地电磁数据的限制。地震剖面描述了从邦迪向东南方向的Vindhyan层序逐渐增厚。上部和下部Vindhyans的速度分别为4.6 a,“ 4.8 km / s和5.1 a”。 “ 5.3 km /s。Vindhyan盆地的西北边界由大边界断层(GBF)划定,该边界表现为一个30 k​​m宽的NW俯冲断层,延伸至30 km的深度。

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