Abstract

Multi-scale bedding fractures, i.e., km-scale regional bedding fractures and cm-scale lamina-induced fractures, have been the focus of unconventional oil and gas exploration and play an important role in resource exploration and drilling practice for tight oil and gas. It is challenging to conduct numerical simulations of bedding fractures due to the strong heterogeneity without a proper mechanical criterion to predict failure behaviors. This research modified the Tien–Kuo (T–K) criterion by using four critical parameters (i.e., the maximum principal stress (σ1), minimum principal stress (σ3), lamina angle (θ), and lamina friction coefficient (μlamina)). The modified criterion was compared to other bedding failure criteria to make a rational finite element simulation constrained by the four variables. This work conducted triaxial compression tests of 18 column samples with different lamina angles to verify the modified rock failure criterion, which contributes to the simulation work on the multi-scale bedding fractures in the statics module of the ANSYS workbench. The cm-scale laminated rock samples and the km-scale Yanchang Formation in the Ordos Basin were included in the multi-scale geo-models. The simulated results indicate that stress is prone to concentrate on lamina when the lamina angle is in an effective range. The low-angle lamina always induces fractures in an open state with bigger failure apertures, while the medium-angle lamina tends to induce fractures in a shear sliding trend. In addition, the regional bedding fractures of the Yanchang Formation in the Himalayan tectonic period tend to propagate under the conditions of lower maximum principal stress, higher minimum principal stress, and larger stratigraphic dip.

Highlights

  • The lamina-induced fractures correspond to the km-scale regional bedding fractures, which are induced by the formation beddings

  • It has been found that the open state of bedding fractures in complicated tectonic zones could play an essential role in oil and gas diffusion, emission, migration, and accumulation [14,17,28,29,30,31,32,33]

  • A finite finite element elementsimulation simulationofoflamina-induced lamina-inducedfractures fractures conducted in the statics module of is is conducted in the statics module of the the ANSYS

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Summary

Introduction

Multi-scale bedding fractures, including km-scale regional bedding fractures and cm-scale lamina-induced fractures, are caused by lamina dissolution or induced by regional tectonic stress [1,2,3,4,5,6,7,8,9,10].The formation of sedimentary lamina and bedding underground exerts a strong control on the following fracture propagation [11,12,13], so the term lamina-induced fractures is used to indicate the cm-scaleEnergies 2020, 13, 131; doi:10.3390/en13010131 www.mdpi.com/journal/energiesEnergies 2020, 13, 131 fractures forming along the core lamina under the influence of external forces and internal rock mechanical properties [14]. The lamina-induced fractures correspond to the km-scale regional bedding fractures, which are induced by the formation beddings These fractures have been the focus of conventional and unconventional oil and gas reservoir characterization including shale, tight oil [14,15,16,17,18,19,20,21,22,23], and Carboniferous rocks [24]. It has been found that the open state of bedding fractures in complicated tectonic zones could play an essential role in oil and gas diffusion, emission, migration, and accumulation [14,17,28,29,30,31,32,33]. The lamina or bedding in the tight reservoirs coupled with the hydraulic fractures could induce a more complicated in-situ fracture network [34]

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