Miocene mass-transport sediments, Troodos Massif, Cyprus

被引：15

作者：

Lord, Alan R. ^{[1
,2
]}

Harrison, Richard W. ^{[3
]}

BouDagher-Fadel, Marcelle ^{[4
]}

Stone, Byron D. ^{[3
]}

Varol, Osman ^{[5
]}

机构：

[1] Senckenberg Forschungsinst, D-60325 Frankfurt, Germany

[2] Natl Museum, D-60325 Frankfurt, Germany

[3] US Geol Survey, Eastern Geol & Climate Sci Ctr, Natl Ctr, Reston, VA 20192 USA

[4] UCL, Dept Earth Sci, London WC1E 6BT, England

[5] Varol Res Ltd, Rhos On Sea LL28 4AE, Wales

来源：

PROCEEDINGS OF THE GEOLOGISTS ASSOCIATION | 2009年 / 120卷

关键词：

Miocene; Pakhna Formation; Cyprus; Hemipelagic sediments; Mass-transport; Planktonic microfossils; MESSINIAN SALINITY CRISIS; SOUTHERN CYPRUS; SOUTHWEST CYPRUS; MAMONIA COMPLEX; PISSOURI BASIN; EVOLUTION; HISTORY; TECTONICS; FRAMEWORK; UPLIFT;

D O I：

10.1016/j.pgeola.2009.08.001

中图分类号：

P5 [地质学];

学科分类号：

0709 ; 081803 ;

摘要：

Sediment mass-transport layers Of Submarine origin on the northern and southern flanks of the Troodos ophiolitic massif are dated biostratigraphically as early Miocene and late Miocene, respectively and therefore represent different seismogenic events in the uplift and erosional history of the Troodos terrane. Analysis of such events has potential for documenting Miocene seismic and uplift events regionally in the context of changing stress field directions and plate vectors through time. (C) 2009 The Geologists' Association. Published by Elsevier Ltd. All rights reserved.

引用

页码：133 / 138

页数：6

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