Results 91 to 100 of about 25,421 (273)

Ophiolite Metamorphism and Ocean-Floor Metamorphism.

open access: yesJournal of Geography (Chigaku Zasshi), 1995
Ophiolites of primary igneous origin have been more or less modified by later metamorphic processes, and there are several types of ophiolite metamorphism such as (1) the low-pressure type as recognized in ophiolites of the Mediterranean, Alps, Oman, Newfoundland, Chile, Taiwan, Borneo, California Coast Range, Hidaka Western Zone, and Horokanai, (2 ...
ISHIZUKA, Hideo, SUZUKI, Satoko
openaire   +2 more sources

The structural, metamorphic and thermal history of the Sonnblick Dome, southeast Tauern Window, Austria [PDF]

open access: yes, 1990
Within the southeastern Tauern Window, the Sonnblick Dome is a large, NE-verging, antiformal structure composed of orthogneisses of the Zentralgneis Complex.
Reddy, Steven Michael
core  

Identifying airborne snow metamorphism with stable water isotopes [PDF]

open access: yes
<jats:p>Abstract. Wind-blown snow is a frequent phenomenon in high-elevation and polar regions which impacts the surface energy and mass balance of these areas.
Wahl, Sonja   +4 more
core   +1 more source

metamorphism and deformation in the Belledonne Massif (Western Alps)

open access: yes, 2021
The age and P–T conditions of Variscan high-P(HP) metamorphism in the Palaeozoic basement of the western Alps remain poorly constrained, but is nevertheless crucial to build a consistent tectonic scenario for the southeastern domain of the Variscan Belt.
Stéphane Guillot   +11 more
core   +1 more source

Confirmation of the impact origin of the Late Ordovician Tvären impact structure (southeast Sweden) and emplacement of impactites in a marine setting

open access: yesMeteoritics &Planetary Science, EarlyView.
Abstract The Tvären structure in southeastern Sweden has been listed as a confirmed marine‐target impact structure for decades. However, to date, no measurements and/or indexed data of planar deformation features in quartz grains from the structure have been published or any other unequivocal evidence of impact.
Katarzyna J. Gajewska   +6 more
wiley   +1 more source

Geochronological and structural constraints on the Cretaceous thermotectonic evolution of the Kraishte zone (Western Bulgaria) [PDF]

open access: yes, 2010
In the Kraishte region, near the junction of the Balkanides and Dinarides, late Early Cretaceous compression led to the thrusting of the Morava unit over the Struma unit.
Bernoulli, D.   +5 more
core   +1 more source

Polymict melt‐bearing breccia dikes in the Morokweng impact structure formed by slip‐induced mechanical mixing of pseudotachylite and cataclasite along large‐displacement impact faults

open access: yesMeteoritics &Planetary Science, EarlyView.
Abstract A core drilled through shocked and faulted Archean granitoid gneisses and dolerites in the eroded peak ring of the 70–80 km diameter Morokweng impact structure intersects multiple centimeter‐ to meter‐wide clastic‐matrix breccias containing a polymict clast population of lithic and mineral clasts and altered, millimeter‐ to centimeter ‐size ...
Roger L. Gibson   +3 more
wiley   +1 more source

A Metamorphic Lesion [PDF]

open access: yesGastroenterology, 2009
Rolanda, C, Gonçalves, R, Macedo, G
openaire   +4 more sources

Thermal structure of the crust during granulite metamorphism: petrological speculations and geodynamic implications

open access: yes, 1998
P(論文)It is shown on a basis of generalization of lateral and vertical distribution of P-T parameters in granulite-gneiss belts of various ages that the thermal gradient within the lower crust during granulite metamorphism is rather low, ca. 5-10℃/km. Two
Mints,Michael V., Konilov,Alexander N.
core  

Alpine Metamorphism of Mafic Rocks

open access: yes, 1974
Metamorphosed mafic rocks in the Alps exhibit many characteristic mineral assemblages. They are used to study different phases of alpine metamorphism. The great variety of alpine metamorphosed mafic and ultramafic rocks is illustrated with a map of their
Vuagnat, Marc   +2 more
core   +1 more source

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