Universität zu Köln

Pourteau, Amaury ORCID: 0000-0002-6121-8383, Scherer, Erik E., Schorn, Simon, Bast, Rebecca, Schmidt, Alexander and Ebert, Lisa (2019). Thermal evolution of an ancient subduction interface revealed by Lu-Hf garnet geochronology, Halilbagi Complex (Anatolia). Geosci. Front., 10 (1). S. 127 - 149. HAIDIAN DISTRICT: CHINA UNIV GEOSCIENCES, BEIJING. ISSN 1674-9871

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Abstract

The thermal structure of subduction zones exerts a major influence on deep-seated mechanical and chemical processes controlling arc magmatism, seismicity, and global element cycles. Accretionary complexes exposed inland may comprise tectonic blocks with contrasting pressure-temperature (P-T) histories, making it possible to investigate the dynamics and thermal evolution of former subduction interfaces. With this aim, we present new Lu-Hf geochronological results for mafic rocks of the Halilbagi Complex (Anatolia) that evolved along different thermal gradients. Samples include a lawsonite-epidote blueschist, a lawsonite-epidote eclogite, and an epidote eclogite (all with counter-clockwise P-T paths), a prograde lawsonite blueschist with a hairpin-type P-T path, and a garnet amphibolite from the overlying sub-ophiolitic metamorphic sole. Equilibrium phase diagrams suggest that the garnet amphibolite formed at similar to 0.6-0.7 GPa and 800-850 degrees C, whereas the prograde lawsonite blueschist records burial from 2.1 GPa and 420 degrees C to 2.6 GPa and 520 degrees C. Well-defined Lu-Hf isochrons were obtained for the epidote eclogite (92.38 +/- 0.22 Ma) and the lawsonite-epidote blueschist (90.19 +/- 0.54 Ma), suggesting rapid garnet growth. The lawsonite-epidote eclogite (87.30 +/- 0.39 Ma) and the prograde lawsonite blueschist (ca. 86 Ma) are younger, whereas the garnet amphibolite (104.5 +/- 3.5 Ma) is older. Our data reveal a consistent trend of progressively decreasing geothermal gradient from granulite-facies conditions at similar to 104 Ma to the epidote-eclogite facies around 92 Ma, and the lawsonite blueschist-facies between 90 Ma and 86 Ma. Three Lu-Hf garnet dates (between 92 Ma and 87 Ma) weighted toward the growth of post-peak rims (as indicated by Lu distribution in garnet) suggest that the HP/LT rocks were exhumed continuously and not episodically. We infer that HP/LT metamorphic rocks within the Halilbagi Complex were subjected to continuous return flow, with warm rocks being exhumed during the tectonic burial of cold ones. Our results, combined with regional geological constraints, allow us to speculate that subduction started at a transform fault near a mid-oceanic spreading centre. Following its formation, this ancient subduction interface evolved thermally over more than 15 Myr, most likely as a result of heat dissipation rather than crustal underplating. (C) 2018, China University of Geosciences (Beijing) and Peking University. Production and hosting by Elsevier B.V.

Item Type:	Journal Article
Creators:	Creators Email ORCID ORCID Put Code Pourteau, Amaury UNSPECIFIED orcid.org/0000-0002-6121-8383 UNSPECIFIED Scherer, Erik E. UNSPECIFIED UNSPECIFIED UNSPECIFIED Schorn, Simon UNSPECIFIED UNSPECIFIED UNSPECIFIED Bast, Rebecca UNSPECIFIED UNSPECIFIED UNSPECIFIED Schmidt, Alexander UNSPECIFIED UNSPECIFIED UNSPECIFIED Ebert, Lisa UNSPECIFIED UNSPECIFIED UNSPECIFIED
URN:	urn:nbn:de:hbz:38-140970
DOI:	10.1016/j.gsf.2018.03.004
Journal or Publication Title:	Geosci. Front.
Volume:	10
Number:	1
Page Range:	S. 127 - 149
Date:	2019
Publisher:	CHINA UNIV GEOSCIENCES, BEIJING
Place of Publication:	HAIDIAN DISTRICT
ISSN:	1674-9871
Language:	English
Faculty:	Unspecified
Divisions:	Unspecified
Subjects:	no entry
Uncontrolled Keywords:	Keywords Language RB-SR GEOCHRONOLOGY; METAMORPHIC SOLE; INTRAOCEANIC SUBDUCTION; SIVRIHISAR MASSIF; TAVSANLI ZONE; SM-ND; AR-40-AR-39 GEOCHRONOLOGY; PROGRADE METAMORPHISM; FRANCISCAN SUBDUCTION; OPHIOLITIC MELANGE Multiple languages Geosciences, Multidisciplinary Multiple languages
Refereed:	Yes
URI:	http://kups.ub.uni-koeln.de/id/eprint/14097