首页> 外文期刊>International Journal of Rock Mechanics and Mining Sciences >Geomechanical modeling using finite element method for prediction of in-situ stress in Krishna-Godavari basin, India
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Geomechanical modeling using finite element method for prediction of in-situ stress in Krishna-Godavari basin, India

机译:印度克里希纳-哥达瓦里盆地有限元地质力学建模预测地应力

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This study provides quantitative rock mechanical properties and analyses of in-situ stress and pore pressure in several oil/gas fields of East and West Godavari sub-basins. High pore pressure gradients varying from 11.85 to 12.80 MPa/km exist within these oil/gas fields. Vertical stress (St) gradients in the range 21.00 to 22.85 MPa/km are seen to exist. Minimum horizontal principal stress (SO magnitude is found to vary from 64% to 76% of S-v, while maximum horizontal principal stress (511) magnitude is observed to vary from 90% to 92% of S-v within normally pressured to over-pressured sediments. The breakout derived S-H, orientation from two well varies from N14 degrees E to N22.5 degrees E in the Krishna-Godavari basin. Rock mechanical properties such as Young's modulus, Poisson's ratio and unconfined compressive strength have been estimated from logs of compressional and shear wave travel time. Two-dimensional (2D) stress modeling using finite element analysis has been carried out for some important oil/gas fields situated within East and West Godavari sub-basins as a part of the current study. Regional SH orientation has been used for application of stress at the model boundary. Discontinuities in the stress pattern which can be associated with interfaces between weak and competent layers have been commonly observed and especially where silici-clastic and volcanic inter-bedded sequences are encountered. The model predicted stress orientations are verified with the Formation Micro Imager (FMI) log data of wells at the above-mentioned sub-basins. (C) 2014 Elsevier Ltd. All rights reserved
机译:这项研究提供了定量的岩石力学特性,并分析了东西方戈达瓦里子盆地几个油气田的地应力和孔隙压力。在这些油气田中存在高孔隙压力梯度,范围从11.85至12.80 MPa / km。可以看到在21.00至22.85 MPa / km的范围内存在垂直应力(St)梯度。在常压至超压沉积物中,最小水平主应力(SO大小在Sv的64%到76%之间变化),而最大水平主应力(511)在Sv的90%到92%之间变化。克里希纳-哥达瓦里盆地从两口井的破裂中得到的SH取向从N14度E到N22.5度E变化,岩石的力学特性如杨氏模量,泊松比和无侧限抗压强度通过压缩和剪切测井估算得出波传播时间,作为研究的一部分,已经对东西戈达瓦里子盆地和东西戈达瓦里子盆地内的一些重要油气田进行了使用有限元分析的二维(2D)应力建模,并使用了区域SH方向应力模式的不连续性可能与薄弱层和有效层之间的界面有关,这种现象通常被观察到,特别是遇到硅碎屑和火山夹层层序的地方。使用上述子盆地的井的地层显微成像仪(FMI)测井数据验证了模型预测的应力方向。 (C)2014 Elsevier Ltd.保留所有权利

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