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Palaeozoic Collision Between the North and South China Blocks, Triassic Intracontinental Tectonics, and the Problem of the Ultrahigh-Pressure Metamorphism [PDF]

open access: yesComptes Rendus - Geoscience, 2008
International audienceThe Qinling–Dabie Belt represents the boundary between the North and South China Blocks (NCB, SCB, respectively), where ultrahigh-pressure (UHP) rocks are widespread.
Michel Faure   +2 more
exaly   +3 more sources

Extensional deformation of post ultrahigh-pressure metamorphism and exhumation process of ultrahigh-pressure metamorphic rocks in the Dabie massif, China

Science in China Series D: Earth Sciences, 2000
A detailed tectonic analysis demonstrates that the present observed regional tectonic configuration of the ultrahigh-pressure metamorphic terrane in the Dabie massif was mainly formed by the extension processes of the post-Indosinian continent-continent oblique collision between the Sino-Korean and Yangtze cratons and ultrahigh-pressure metamorphism ...
Shutian Suo, Zengqiu Zhong, Zhendong You
openaire   +1 more source

Evidence for ultrahigh-pressure metamorphism discovered in the Appalachian orogen

Geology, 2020
AbstractThe Appalachian orogen has long been enigmatic because, compared to other parts of the Paleozoic orogens that formed following the subduction of the Iapetus Ocean, direct evidence for ultrahigh-pressure (UHP) metamorphism has never been found.
Joseph P. Gonzalez   +4 more
openaire   +1 more source

The Realm of Ultrahigh-Pressure Metamorphism

Elements, 2013
The discovery of diamond and coesite in crustal rocks is compelling evidence that continental material has experienced pressures that can only be achieved at mantle depths. At least 20 terranes of unequivocal continental crust containing diamond or coesite are now recognized around the globe; their study constitutes a new field in petrology called ...
openaire   +1 more source

Microdiamonds in Ultrahigh-Pressure Metamorphic Rocks

Elements, 2005
Since the first report of microdiamonds of metamorphic origin in crustal rocks of the Kokchetav Massif, northern Kazakhstan, diamonds have been described from several other ultrahigh-pressure (UHP) metamorphic terranes. In situ diamond is the best indicator of ultrahigh-pressure conditions (>4 GPa), and testifies to subduction of continental crust to ...
openaire   +1 more source

Ultrahigh‐pressure metamorphism at the Lanterman Range (northern Victoria Land, Antarctica)

Geological Journal, 2011
AbstractNorthern Victoria Land is a key area for the Ross Orogen—a Palaeozoic fold belt formed at the palaeo‐Pacific margin of Gondwana and also known as the Delamerian and Tyennan Orogeny in southern Australia, and Tasmania, respectively. A narrow and discontinuous high‐ to ultrahigh‐pressure (HP/UHP) belt, consisting of mafic and ultramafic rocks ...
PALMERI, R.   +2 more
openaire   +2 more sources

Elastic and Seismic Properties of Dabie‐Sulu Ultrahigh Pressure Metamorphic Rocks

Acta Geologica Sinica - English Edition, 2012
Abstract:Lamé modulus (λ) and shear modulus (μ) are among the most important, intrinsic, elastic constants of rocks. Using λ and μ could be much more advantageous than using P‐ and S‐wave velocities (Vp and Vs). Here we quantified these equivalent isotropic elastic moduli for 115 representative rocks from the ultrahigh pressure (UHP) metamorphic ...
WANG Qian   +4 more
openaire   +2 more sources

High- and ultrahigh-pressure metamorphism from microscopic to orogenic scale

Lithos, 2015
This volume includes contributions presented during the 10th International Eclogite Conference held in Courmayeur, Italy, September 2nd-10th ...
Castelli D.   +3 more
openaire   +2 more sources

Lithospheric seismic fabrics of Sulu ultrahigh-pressure metamorphic belt

Science in China Series D: Earth Sciences, 2005
Calibration of seismic reflectors appearing in the crust of the Chinese continent scientific drilling site can be completed through the correlation studies between direct evidences, such as the drill cores, and geophysical signatures; therefore the interpretation of geophysical data could produce reliable results of crustal structure and composition ...
Wencai Yang   +3 more
openaire   +1 more source

Exhumation of high- and ultrahigh-pressure metamorphic rocks by slab extraction

Geology, 2003
Exhumation of high- and ultrahigh-pressure metamorphic rocks in collisional orogens may be explained by upward extrusion of these rocks, erosion of their overburden, or extensional thinning of the overburden. Some high-pressure terranes, such as the Adula nappe in the Central Alps, fit none of these scenarios. We propose an additional way in which part
Nikolaus Froitzheim   +3 more
openaire   +1 more source

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