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Relationship amongst gravity gradients, deflection of vertical, Moho deflection and the stresses derived by mantle convections : a case study over Indo-Pak and surroundings

机译:重力梯度,垂向挠度,莫霍面挠度与地幔对流所产生的应力之间的关系:以印巴和周边地区为例

摘要

All  quantities,  which are  measured  in  the  gravity  field  of  the  Earth are affected by  the  field,  therefore,  there should  be correlations  amongst  them.  Here,  we  focus  on  some  gravimetrically-determined  quantities  like  deflections  of  vertical, deflections of Moho, vertical-horizontal gravity gradients and the shear sub-lithospheric stress components due to mantle convection. We show that how these quantities are related to each other mathematically so that one of them can be written in term of another. This somehow proves the presence of the mentioned correlations theoretically. Also, we generate the maps of these quantities over the Indo-Pak and surrounding areas and show how similar they are. Thereafter, they are explained and  interpreted  geologically.  Our  investigations  show  that  the  maps  of  these  quantities  are  in  good  agreements  with topographic and geological features. The map of the vertical-horizontal gravity gradients shows more detailed information of the  gravity field due to  signal amplification at high  degrees,  that of Moho deflection shows sub-surface features due to reduction of the effect of topographic masses. The map of the shear sub-lithospheric stress components is much smoother than the gradients, as expected, and has good agreement with the collisional and subduction zones as well.  Relationship amongst gravity gradients, deflection of vertical, Moho deflection and the stresses derived by mantle convections-a case study over Indo-Pak and surroundings. Available from: https://www.researchgate.net/publication/292538682_Relationship_amongst_gravity_gradients_deflection_of_vertical_Moho_deflection_and_the_stresses_derived_by_mantle_convections-a_case_study_over_Indo-Pak_and_surroundings [accessed Feb 1, 2016].
机译:在地球的重力场中测量的所有数量都受该场的影响,因此,它们之间应具有相关性。在这里,我们重点关注一些由重量法确定的量,例如垂直偏转,莫霍(Moho)偏转,垂直水平重力梯度以及由于地幔对流而引起的地下岩层切变应力分量。我们证明了这些量在数学上是如何相互关联的,从而可以用另一个来写一个。这从理论上证明了上述相关性的存在。此外,我们还会在印巴和周边地区生成这些数量的地图,并显示它们的相似程度。此后,对它们进行地质解释和解释。我们的调查表明,这些数量的地图具有良好的协议,具有地形和地质特征。垂直水平重力梯度的地图显示了由于高度信号放大而引起的重力场的更详细信息,而Moho偏转的重力场则显示了由于地形质量的影响减小而引起的地下特征。如预期的那样,剪切下岩石圈应力分量的映射比梯度平滑得多,并且与碰撞区和俯冲区也具有很好的一致性。重力梯度,垂直挠度,莫霍挠度和地幔对流所产生的应力之间的关系-以印度-北和周围地区为例。可从以下网址获得:https://www.researchgate.net/publication/292538682_Relationship_amongst_gravity_gradients_deflection_of_vertical_Moho_deflection_and_the_stresses_derived_by_mantle_convections-a_case_study_over_Indo-Pak_and_surroundings [请访问2月1日,

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