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Journal ArticleDOI

Jadeite–chloritoid–glaucophane–lawsonite blueschists in north-west Turkey: unusually high P/T ratios in continental crust

Aral I. Okay
- 01 Nov 2002 - 
- Vol. 20, Iss: 8, pp 757-768
TLDR
Sodic metapelites with jadeite, chloritoid, glaucophane and lawsonite formed a coherent regional metamorphic sequence, several tens of square kilometres in size, and over a kilometre thick, in the Orhaneli region of northwest Turkey as mentioned in this paper.
Abstract
Sodic metapelites with jadeite, chloritoid, glaucophane and lawsonite form a coherent regional metamorphic sequence, several tens of square kilometres in size, and over a kilometre thick, in the Orhaneli region of northwest Turkey. The low-variance mineral assemblage in the sodic metapelites is quartz + phengite + jadeite + glaucophane + chloritoid + lawsonite. The associated metabasites are characterized by sodic amphibole + lawsonite ± garnet paragenesis. The stable coexistence of jadeite + chloritoid + glaucophane + lawsonite, not reported before, indicates metamorphic pressures of 24 ± 3 kbar and temperatures of 430 ± 30  °C for the peak blueschist facies conditions. These P–T conditions correspond to a geotherm of 5  °C km−1, one of the lowest recorded in continental crustal rocks. The low geotherm, and the known rate of convergence during the Cretaceous subduction suggest low shear stresses at the top of the downgoing continental slab.

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Citations
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Journal ArticleDOI

Metamorphic Conditions in Orogenic Belts: A Record of Secular Change

TL;DR: The abundance and scale of ultra-high-temperature (UHT) metamorphic belts from the Neoarchean to the Cambrian imply a significant change in geodynamics during the Neo-Archean Era, after which transient sites of high heat flow were available at intervals throughout this period of Earth evolution as mentioned in this paper.
Journal ArticleDOI

Very-low-temperature record of the subduction process: A review of worldwide lawsonite eclogites

TL;DR: Lawsonite eclogites preserve a record of very low-temperature conditions in subduction zones as mentioned in this paper, typically characterized by accretionary complexes lithologies and as tectonic blocks within serpentinite-matrix melange.
Journal ArticleDOI

Tectonic units of the Alpine collision zone between Eastern Alps and western Turkey

TL;DR: In this article, a map that correlates tectonic units between Alps and western Turkey accompanied by a text providing access to literature data is presented, explaining the concepts used for defining the mapped Tectonic Units, and first-order paleogeographic inferences.
References
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Journal ArticleDOI

An internally consistent thermodynamic data set for phases of petrological interest

TL;DR: In this paper, the thermodynamic properties of 154 mineral endmembers, 13 silicate liquid end-members and 22 aqueous fluid species are presented in a revised and updated data set.

An internally consistent thermodynamic data set for phases of petrological interest

J. B. H Olland, +1 more
TL;DR: In this article, the authors presented a revised and updated data set of 154 mineral end-members, 13 silicate liquid endmembers and 22 aqueous fluid species, which is used for the calculation of uncertainties on mineral reactions to be performed.
Journal ArticleDOI

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TL;DR: In this paper, the authors bring together information from various fields of science to produce an overview of one of the world's complex orogenic areas, namely the eastern Mediterranean, to study the processes of continental rifting, passive margin development, ophiolite generation and emplacement and the tectonic, magmatic and sedimentary effects of continental collision.
Journal ArticleDOI

Phase relations of epidote-blueschists

TL;DR: In this paper, phase diagrams have been computed for minerals in the system NCMASH, using the optimised thermodynamic data-base of Berman (1988) augmented by data on glaucophane and pumpellyite, to illustrate the relationships between rocks containing epidote and sodic amphibole and those containing assemblages characteristic of neighbouring metamorphic facies.
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