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Subduction and closure of the Palaeo...

Eizenhofer, Paul R.

Subduction and closure of the Palaeo-Asian Ocean along the Solonker Suture Zoneconstraints from an integrated sedimentary provenance analysis /

Record Type:	Electronic resources : Monograph/item
Title/Author:	Subduction and closure of the Palaeo-Asian Ocean along the Solonker Suture Zoneby Paul R. Eizenhofer.
Reminder of title:	constraints from an integrated sedimentary provenance analysis /
Author:	Eizenhofer, Paul R.
Published:	Singapore :Springer Singapore :2020.
Description:	xxxv, 270 p. :ill. (some col.), digital ;24 cm.
Contained By:	Springer eBooks
Subject:	Geology, StructuralEast Asia.
Online resource:	https://doi.org/10.1007/978-981-32-9200-0
ISBN:	9789813292000$q(electronic bk.)

Subduction and closure of the Palaeo-Asian Ocean along the Solonker Suture Zoneconstraints from an integrated sedimentary provenance analysis /
Eizenhofer, Paul R.

Subduction and closure of the Palaeo-Asian Ocean along the Solonker Suture Zoneconstraints from an integrated sedimentary provenance analysis /[electronic resource] :by Paul R. Eizenhofer. - Singapore :Springer Singapore :2020. - xxxv, 270 p. :ill. (some col.), digital ;24 cm. - Springer theses,2190-5053. - Springer theses..

Introduction -- Regional Geology across the Solonker Suture Zone -- Methodology -- Results -- Geochronological Entropy, and its Relevance to Age Measurements -- Accretionary Collision between the Mongolian Arcs and North China Craton -- Conclusions.

This Ph.D. thesis attempts to decipher the closure of the Palaeozoic Palaeo-Asian Ocean along the enigmatic Solonker Suture in East Asia adopting a methodology that integrates geochemical and geochronological data from Palaeozoic sedimentary and volcanic rocks in the region. It provides an in-detail but also broad insight into the Palaeozoic to early Mesozoic tectonic evolution of the region, not only pin-pointing the debated location of the Solonker Suture but also the timing of final disappearance of the Palaeo-Asian Ocean during Permian to Early Triassic times. The results have led to propose a tectonic 'soft-collision' model for the amalgamation of the North China Craton and the Mongolian Terranes in northern Asia explaining the general absence of geologic features characteristic for continent-continent collisions such as the occurrence of regional-scale high-grade metamorphic rocks, ophiolite belts and fold-thrust structures. This new model may serve as a blueprint for the tectonic evolution of similar suture zones that are characterized by the absence of typical collision related lithologies and structures. The thesis is particularly useful as a guide for researchers who seek an in-depth understanding of the Palaeozoic to early Mesozoic tectonic evolution of northern China and Central Asia along the Solonker Suture.

ISBN: 9789813292000$q(electronic bk.)

Standard No.: 10.1007/978-981-32-9200-0doiSubjects--Topical Terms:

864818
Geology, Structural
--East Asia.

LC Class. No.: QE634.E18

Dewey Class. No.: 551.8

Subduction and closure of the Palaeo-Asian Ocean along the Solonker Suture Zoneconstraints from an integrated sedimentary provenance analysis /
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520 $a This Ph.D. thesis attempts to decipher the closure of the Palaeozoic Palaeo-Asian Ocean along the enigmatic Solonker Suture in East Asia adopting a methodology that integrates geochemical and geochronological data from Palaeozoic sedimentary and volcanic rocks in the region. It provides an in-detail but also broad insight into the Palaeozoic to early Mesozoic tectonic evolution of the region, not only pin-pointing the debated location of the Solonker Suture but also the timing of final disappearance of the Palaeo-Asian Ocean during Permian to Early Triassic times. The results have led to propose a tectonic 'soft-collision' model for the amalgamation of the North China Craton and the Mongolian Terranes in northern Asia explaining the general absence of geologic features characteristic for continent-continent collisions such as the occurrence of regional-scale high-grade metamorphic rocks, ophiolite belts and fold-thrust structures. This new model may serve as a blueprint for the tectonic evolution of similar suture zones that are characterized by the absence of typical collision related lithologies and structures. The thesis is particularly useful as a guide for researchers who seek an in-depth understanding of the Palaeozoic to early Mesozoic tectonic evolution of northern China and Central Asia along the Solonker Suture.
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