Kinematics of transform and transcurrent faults

Freund, Raphael

doi:10.1016/0040-1951(74)90064-x

Cited by 363 publications

(128 citation statements)

References 16 publications

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“…Falvey 1974;Veevers 1981;Buck 1991;Menzies et al 2002;Manatschal 2004;Huismans & Beaumont 2005, transform margins (see the models of Wilson 1965;Freund 1974;Mascle 1976;Mascle & Blarez 1987) and oblique margins (e.g. Cochran 1973;Sims et al 1999;Bird 2001;Clifton & Schlische 2001;d'Acremont et al 2006;Lizarralde et al 2007).…”

Section: Dynamic Developmentmentioning

confidence: 99%

Transform margins: development, controls and petroleum systems – an introduction

Němčok

Rybár

Sinha

et al. 2016

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This paper provides an overview of the existing knowledge of transform margins including their dynamic development, kinematic development, structural architecture and thermal regime, together with the factors controlling these. This systematic knowledge is used for describing predictive models of various petroleum system concept elements such as source rock, seal rock and reservoir rock distribution, expulsion timing, trapping style and timing, and migration patterns. The paper then introduces individual contributions to this volume and their focus.

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Section: Dynamic Developmentmentioning

confidence: 99%

Transform margins: development, controls and petroleum systems – an introduction

Němčok

Rybár

Sinha

et al. 2016

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“…We tentatively interpret these latter data as reflecting localized sinistral shear within this strongly deformed zone. Another explanation could be localized pure shear, in which some blocks undergo CCW rotation [Freund, 1974].…”

Section: Go•tanj Fault and Velenje Basinmentioning

confidence: 99%

Miocene‐Pliocene tectonic evolution of the Slovenian Periadriatic fault: Implications for Alpine‐Carpathian extrusion models

Jelen²,

et al. 1998

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Abstract. The Periadriatic Line (PAL) is a remarkable, several hundred kilometer long fault system of the Alpine orogen. Its dextral character was documented by several authors using diverse criteria, but detailed kinematics and timing of movements had not been investigated along its whole length. Structural and paleomagnetic measurements, mapping, and stratigraphic and sedimentological studies have helped to unravel the MiocenePliocene evolution of the Slovenian segment of the PAL.

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“…The simplest example of this is 60 a pair of conjugate faults (e.g. Freund, 1974;Nicol et al, 1995;Zhao and 61 Johnson, 1991; Kelly et al, 1998). 62 This paper seeks to extend and develop such studies to large fault networks, 63 within which deformation may be distributed with varying degrees of 64 heterogeneity as a result of the interaction and localization of displacement 65 and strain (e.g.…”

mentioning

confidence: 99%

Deformation within a strike-slip fault network at Westward Ho!, Devon U.K.: Domino vs conjugate faulting

Nixon

Sanderson

Bull

2011

Journal of Structural Geology

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Kinematics of transform and transcurrent faults

Cited by 363 publications

References 16 publications

Transform margins: development, controls and petroleum systems – an introduction

Transform margins: development, controls and petroleum systems – an introduction

Miocene‐Pliocene tectonic evolution of the Slovenian Periadriatic fault: Implications for Alpine‐Carpathian extrusion models

Deformation within a strike-slip fault network at Westward Ho!, Devon U.K.: Domino vs conjugate faulting

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