Incipient continental collision and plate-boundary curvature: Late Pliocene - Holocene transtenstional Hellenic forearc, Crete, Greece

J.H. ten Veen; K.L. Kleinspehn

doi:10.1144/0016-764902-067

Incipient continental collision and plate-boundary curvature: Late Pliocene - Holocene transtenstional Hellenic forearc, Crete, Greece

J.H. ten Veen, K.L. Kleinspehn

Research output: Contribution to Journal › Article › Academic › peer-review

Abstract

Geodynamic controls on Late Pliocene-Holocene kinematics of the Hellenic forearc are assessed using the fan-deltaic basin fill of the Messaras forearc basin of south-central Crete. Previously unrecognized 070° sinistral faults developed in wrench-dominated transtension with strike-slip:normal-slip ratios of 10:1 to 100:1. Coeval folds developed in proximity to the 070° sinistral faults during deposition of the Galini Formation, making them candidates to have developed in transtension, and new chronostratigraphic and

Original language	English
Pages (from-to)	1-21
Number of pages	21
Journal	Journal of the Geological Society (London)
Volume	160
DOIs	https://doi.org/10.1144/0016-764902-067
Publication status	Published - 2003

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10.1144/0016-764902-067

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title = "Incipient continental collision and plate-boundary curvature: Late Pliocene - Holocene transtenstional Hellenic forearc, Crete, Greece",

abstract = "Geodynamic controls on Late Pliocene-Holocene kinematics of the Hellenic forearc are assessed using the fan-deltaic basin fill of the Messaras forearc basin of south-central Crete. Previously unrecognized 070° sinistral faults developed in wrench-dominated transtension with strike-slip:normal-slip ratios of 10:1 to 100:1. Coeval folds developed in proximity to the 070° sinistral faults during deposition of the Galini Formation, making them candidates to have developed in transtension, and new chronostratigraphic and",

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AB - Geodynamic controls on Late Pliocene-Holocene kinematics of the Hellenic forearc are assessed using the fan-deltaic basin fill of the Messaras forearc basin of south-central Crete. Previously unrecognized 070° sinistral faults developed in wrench-dominated transtension with strike-slip:normal-slip ratios of 10:1 to 100:1. Coeval folds developed in proximity to the 070° sinistral faults during deposition of the Galini Formation, making them candidates to have developed in transtension, and new chronostratigraphic and

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DO - 10.1144/0016-764902-067

M3 - Article

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JF - Journal of the Geological Society (London)

ER -

Incipient continental collision and plate-boundary curvature: Late Pliocene - Holocene transtenstional Hellenic forearc, Crete, Greece

Abstract

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