In the coronitic gabbros of La Bastida (Toledo) several metamorphic corona textures of phlogopite and pargasitic amphibole around ilmenite are developed. The genesis of these coronas is directly linked with the widespread development of coronas around olivine. The metamorphic conditions of these coronas are similar to those produced in the other coronitic textures in olivine, that are the intermediate to low pressure granulitic facies of regional metamorphic peak of the areaEn los gabros coroníticos de La Bastida, Toledo, se desarrollan varias texturas metamórficas coroníticas de de flogopita y anfíbol pargasítica alrededor de ilmenita. La génesis de estas coronas está directamente relacionada con el amplio desarrollo de coronas alrededor d...
Reactions between olivine and plagioclase form kelyphytic corona textures in the Rymmen gabbro, sout...
Olivine hornblendites (cortlandtites) form part of the Montnegre mafic complex related to late-Varis...
The pre-Alpine metamorphic history of basement rocks of the Alpine Betic-Rif orogen is still uncerta...
The Bastida gabbros massif is formed by olivine norites and piroxene gabbronorites. The metamorphic ...
A lenticular-shaped, 40 m thick body of ultramafic amphibolite is hosted in a km-sized metabasite le...
The coronitic meta- melagabbronorites are part of the El Arenal bodies which belong to the El Desti...
Three types of corona textures developed in metagabbros of the Sobrado Unit. Detailed thermobarometr...
HP-HT unit exposed in the core of the Sobrado tectonic window (Órdenes Complex, NW Iberian Massif) c...
Corona structures occur in the upper units (UGAZ and UA) or the Niquelandia mafic-ultramafic complex...
The Proterozoic Mathurapur olivine metagabbros possess several types of coronas due to subsolidus re...
Olivine-plagioclase coronas in metagabbros from the Adirondack Mountains are spatially well-organize...
Coronitic metagabbros occur as small isolated bodies along the contact between the Mariánské Lázně a...
Coronae between olivine and plagioclase are a common replacement texture in mafic rocks by magmatic ...
hypersthene-bearing coronas is unusual in a terrain where epidote- and chlorite-bearing assemblages ...
Corona textures between olivine and plagioclase or orthopyroxene and plagioclase are present in Herc...
Reactions between olivine and plagioclase form kelyphytic corona textures in the Rymmen gabbro, sout...
Olivine hornblendites (cortlandtites) form part of the Montnegre mafic complex related to late-Varis...
The pre-Alpine metamorphic history of basement rocks of the Alpine Betic-Rif orogen is still uncerta...
The Bastida gabbros massif is formed by olivine norites and piroxene gabbronorites. The metamorphic ...
A lenticular-shaped, 40 m thick body of ultramafic amphibolite is hosted in a km-sized metabasite le...
The coronitic meta- melagabbronorites are part of the El Arenal bodies which belong to the El Desti...
Three types of corona textures developed in metagabbros of the Sobrado Unit. Detailed thermobarometr...
HP-HT unit exposed in the core of the Sobrado tectonic window (Órdenes Complex, NW Iberian Massif) c...
Corona structures occur in the upper units (UGAZ and UA) or the Niquelandia mafic-ultramafic complex...
The Proterozoic Mathurapur olivine metagabbros possess several types of coronas due to subsolidus re...
Olivine-plagioclase coronas in metagabbros from the Adirondack Mountains are spatially well-organize...
Coronitic metagabbros occur as small isolated bodies along the contact between the Mariánské Lázně a...
Coronae between olivine and plagioclase are a common replacement texture in mafic rocks by magmatic ...
hypersthene-bearing coronas is unusual in a terrain where epidote- and chlorite-bearing assemblages ...
Corona textures between olivine and plagioclase or orthopyroxene and plagioclase are present in Herc...
Reactions between olivine and plagioclase form kelyphytic corona textures in the Rymmen gabbro, sout...
Olivine hornblendites (cortlandtites) form part of the Montnegre mafic complex related to late-Varis...
The pre-Alpine metamorphic history of basement rocks of the Alpine Betic-Rif orogen is still uncerta...