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Pore pressure distribution of a mega-splay fault system in the Nankai Trough subduction zone: Insight into up-dip extent of the seismogenic zone

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TLDR
In this paper, the pore pressure distribution predicted from a waveform tomography (WT) velocity model was used to interpret the evolution of the Nankai Trough off Kumano, Japan.
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This article is published in Earth and Planetary Science Letters.The article was published on 2014-06-15 and is currently open access. It has received 100 citations till now. The article focuses on the topics: Strike-slip tectonics & Pore water pressure.

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Book

Origin and evolution

TL;DR: This book discusses the evolution of Modern Fishes, the Dinosaur Integument, Mammal-like Reptiles, and Reptiles Return to the Sea.
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Review of major shale-dominated detachment and thrust characteristics in the diagenetic zone: Part I, meso- and macro-scopic scale

TL;DR: In this paper, the authors studied the structural characteristics of shale detachments in the Osen-Roa detachment in Southern Norway and found that the detachment's structural style can vary significantly with the number of competent units within the detachment.
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Identification of the static backstop and its influence on the evolution of the accretionary prism in the Nankai Trough

TL;DR: In this paper, reflection seismic data acquired in the Nankai Trough off the Kii Peninsula was analyzed to reveal the origin of a backstop and its influence on the evolution of the accretionary prism.
References
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The Rock Physics Handbook: Tools for seismic analysis of porous media second edition

TL;DR: In this paper, the authors menyaring sejumlah besar teori latar belakang and hasil laboratorium menjadi serangkaian bab ringkas ying memberikan solusi praktis untuk masalah dalam interpretasi data geofisika.
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Theory of elasticity and consolidation for a porous anisotropic solid

TL;DR: In this paper, the elasticity and consolidation theory of isotropic materials is extended to the general case of anisotropy and the method of derivation is also different and more direct.
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Earthquakes and friction laws

TL;DR: The traditional view of tectonics is that the lithosphere comprises a strong brittle layer overlying a weak ductile layer, which gives rise to two forms of deformation: brittle fracture, accompanied by earth-quakes, in the upper layer, and aseismic ductile flow in the layer beneath as mentioned in this paper.
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