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Structural Aspects of the Intraplate Deformations of the Oceanic Crust North of the Afanasii Nikitin Rise (Inidan Ocean)

机译:Afanasii Nikitin隆起(印度洋)北部洋壳板内形变的结构方面

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On the basis of the tectonic interpretation of the continuous seismic profiling data wiht account for the data of deep seismic sounding,we assessed the structure of the test area Sh-22-I of the Labrador Current in the region of the recent intraplate deformations of the Indian Ocean lithosphere northeast of the Afansii Nikitin Rise(Mid-Indian Basin).The possibility of the existence of wide diffuse sinistral shears over ancient transform faults was revealed,which proves their recent tectonic reactivation.The concept of the significant structure-forming role of the processes of serpentinization of the ultramafic rocks of the lower crust and upper mantle and diagonal shears is developed.We show the complicated tectonic interrelations between the young (recent tectonic) compressional structural pattern and that of the ancient Late Cretaceous spreading in the Mid-Indian Basin.The structural relations between the deep crustal inhomogeneities and their manifestation in the recent compressional structures of the sedimentary cover are illustrated.
机译:根据对连续地震剖面资料的构造解释,并结合深地震测深资料,我们评估了拉布拉多海流近期板内变形区域Sh-22-I测试区域的结构。印度洋岩石圈位于Afansii Nikitin Rise(中印度洋盆地)的东北部。揭示了在古老的转换断裂上存在广泛的弥散性正弦切变的可能性,证明了它们最近的构造活化作用。研究了下地壳和上地幔的超镁铁质岩石的蛇纹石化过程以及对角剪力的发展。盆地。深地壳非均匀性及其在近期压缩中的表现之间的结构关系。示出了沉积物覆盖物的结构。

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