Plio/Quaternary strain of the Sorbas Basin, SE Spain: evidence from sediment deformation structures

AE Mather; RK Westhead

Plio/Quaternary strain of the Sorbas Basin, SE Spain: evidence from sediment deformation structures

AE Mather
, RK Westhead

School of Geography, Earth and Environmental Sciences

Research output: Contribution to journal › Article › peer-review

Abstract

Plio/Quaternary fluvial sandstones and conglomerates within the Sorbas Basin, SE Spain contain a number of well preserved deformation features ranging from relatively small scale faulting, to soft sediment deformation structures (clastic dykes; soft sediment folding; soft sediment mixing bodies) and relatively larger scale syn-sedimentary folding. -from Authors

Original language	English
Pages (from-to)	57-65
Number of pages	0
Journal	Quaternary Proceedings
Volume	3
Issue number	0
Publication status	Published - 1 Jan 1993

Cite this

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title = "Plio/Quaternary strain of the Sorbas Basin, SE Spain: evidence from sediment deformation structures",

abstract = "Plio/Quaternary fluvial sandstones and conglomerates within the Sorbas Basin, SE Spain contain a number of well preserved deformation features ranging from relatively small scale faulting, to soft sediment deformation structures (clastic dykes; soft sediment folding; soft sediment mixing bodies) and relatively larger scale syn-sedimentary folding. -from Authors",

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AU - Mather, AE

AU - Westhead, RK

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N2 - Plio/Quaternary fluvial sandstones and conglomerates within the Sorbas Basin, SE Spain contain a number of well preserved deformation features ranging from relatively small scale faulting, to soft sediment deformation structures (clastic dykes; soft sediment folding; soft sediment mixing bodies) and relatively larger scale syn-sedimentary folding. -from Authors

AB - Plio/Quaternary fluvial sandstones and conglomerates within the Sorbas Basin, SE Spain contain a number of well preserved deformation features ranging from relatively small scale faulting, to soft sediment deformation structures (clastic dykes; soft sediment folding; soft sediment mixing bodies) and relatively larger scale syn-sedimentary folding. -from Authors

M3 - Article

VL - 3

SP - 57

EP - 65

JO - Quaternary Proceedings

JF - Quaternary Proceedings

IS - 0

ER -

Plio/Quaternary strain of the Sorbas Basin, SE Spain: evidence from sediment deformation structures

Abstract

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