Processes in continental collision zones: Preface

Yong-Fei Zheng, Lifei Zhang, William C. McClelland, Simon Cuthbert

Research output: Contribution to journalEditorial

Abstract

Formation and exhumation of high-pressure (HP) to ultrahigh-pressure (UHP) metamorphic rocks in continental subduction zones are the two fundamental geodynamic aspects of collisional orogensis. This volume is based on the Session 08c titled “Geochemical processes in continental collision zones” at Goldschmidt 2010 in Knoxville, USA. It focuses on micro- to macro-scale processes that are temporally and spatially linked to different depths of crustal subduction/exhumation and associated mineralogical changes. They are a key to understanding a wide spectrum of phenomena, involving HP/UHP metamorphism and syn-/post-collisional magmatism. Papers in this volume report progresses in petrological, geochronological and geochemical studies of UHP metamorphic rocks and their derivatives in China, with tectonic settings varying from arc–continent collision to continent–continent collision. Microbeam in-situ analyses of metamorphic and magmatic minerals are successfully utilized to solve various problems in the study of continental deep subduction and UHP metamorphism. In addition to their geochronological applications to dating of HP to UHP metamorphic events during continental collision, microbeam techniques have also served as an efficient means to recognize different generations of mineral growth during continental subduction-zone metamorphism. Furthermore, metamorphic dehydration and partial melting of UHP metamorphic rocks during subduction and exhumation are highlighted with respect to their effects on fluid action and element mobilization. These have provided new insights into chemical geodynamics in continental subduction zones.
Original languageEnglish
Pages (from-to)1-9
JournalLithos
Volume136-139
DOIs
Publication statusPublished - 2012

Fingerprint

collision zone
continental collision
exhumation
metamorphic rock
subduction zone
ultrahigh pressure metamorphism
subduction
Metamorphic rocks
geodynamics
collision
Geodynamics
dehydration melting
mineral
tectonic setting
Minerals
partial melting
mobilization
magmatism
High pressure effects
metamorphism

Cite this

Zheng, Y-F., Zhang, L., McClelland, W. C., & Cuthbert, S. (2012). Processes in continental collision zones: Preface. Lithos, 136-139, 1-9. https://doi.org/Yong-Fei Zheng
Zheng, Yong-Fei ; Zhang, Lifei ; McClelland, William C. ; Cuthbert, Simon. / Processes in continental collision zones : Preface. In: Lithos. 2012 ; Vol. 136-139. pp. 1-9.
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abstract = "Formation and exhumation of high-pressure (HP) to ultrahigh-pressure (UHP) metamorphic rocks in continental subduction zones are the two fundamental geodynamic aspects of collisional orogensis. This volume is based on the Session 08c titled “Geochemical processes in continental collision zones” at Goldschmidt 2010 in Knoxville, USA. It focuses on micro- to macro-scale processes that are temporally and spatially linked to different depths of crustal subduction/exhumation and associated mineralogical changes. They are a key to understanding a wide spectrum of phenomena, involving HP/UHP metamorphism and syn-/post-collisional magmatism. Papers in this volume report progresses in petrological, geochronological and geochemical studies of UHP metamorphic rocks and their derivatives in China, with tectonic settings varying from arc–continent collision to continent–continent collision. Microbeam in-situ analyses of metamorphic and magmatic minerals are successfully utilized to solve various problems in the study of continental deep subduction and UHP metamorphism. In addition to their geochronological applications to dating of HP to UHP metamorphic events during continental collision, microbeam techniques have also served as an efficient means to recognize different generations of mineral growth during continental subduction-zone metamorphism. Furthermore, metamorphic dehydration and partial melting of UHP metamorphic rocks during subduction and exhumation are highlighted with respect to their effects on fluid action and element mobilization. These have provided new insights into chemical geodynamics in continental subduction zones.",
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Zheng, Y-F, Zhang, L, McClelland, WC & Cuthbert, S 2012, 'Processes in continental collision zones: Preface' Lithos, vol. 136-139, pp. 1-9. https://doi.org/Yong-Fei Zheng

Processes in continental collision zones : Preface. / Zheng, Yong-Fei; Zhang, Lifei; McClelland, William C.; Cuthbert, Simon.

In: Lithos, Vol. 136-139, 2012, p. 1-9.

Research output: Contribution to journalEditorial

TY - JOUR

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T2 - Preface

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AU - Cuthbert, Simon

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AB - Formation and exhumation of high-pressure (HP) to ultrahigh-pressure (UHP) metamorphic rocks in continental subduction zones are the two fundamental geodynamic aspects of collisional orogensis. This volume is based on the Session 08c titled “Geochemical processes in continental collision zones” at Goldschmidt 2010 in Knoxville, USA. It focuses on micro- to macro-scale processes that are temporally and spatially linked to different depths of crustal subduction/exhumation and associated mineralogical changes. They are a key to understanding a wide spectrum of phenomena, involving HP/UHP metamorphism and syn-/post-collisional magmatism. Papers in this volume report progresses in petrological, geochronological and geochemical studies of UHP metamorphic rocks and their derivatives in China, with tectonic settings varying from arc–continent collision to continent–continent collision. Microbeam in-situ analyses of metamorphic and magmatic minerals are successfully utilized to solve various problems in the study of continental deep subduction and UHP metamorphism. In addition to their geochronological applications to dating of HP to UHP metamorphic events during continental collision, microbeam techniques have also served as an efficient means to recognize different generations of mineral growth during continental subduction-zone metamorphism. Furthermore, metamorphic dehydration and partial melting of UHP metamorphic rocks during subduction and exhumation are highlighted with respect to their effects on fluid action and element mobilization. These have provided new insights into chemical geodynamics in continental subduction zones.

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