Results 81 to 90 of about 2,386 (223)

On the pseudomorphing of melt-filled pores in migmatites

open access: yes
Pseudomorphs of melt-filled pores, recognized by their generally cuspate shape, are used as diagnostic for the former presence of partial melt. They are commonly observed in migmatites from the mid- to deep crust although they occur in the smaller ...
Sawyer, E. W., Holness, M. B.
core   +1 more source

Oligocene partial melting in the Takab metamorphic complex, NW Iran: Evidence from in situ U-Pb geochronology [PDF]

open access: yesJournal of Sciences, Islamic Republic of Iran, 2013
U-Pb ages obtained on zircons from the investigated migmatites place new constraints on the evolution of the crustal rocks in the Takab area. SHRIMP U-Pb dating of inherited zircon in the melanosome parts of mafic migmatites from the Takab complex gives ...
M. Moazzen
doaj  

Zircon thermometry and U–Pb ion-microprobe dating of the gabbros and associated migmatites of the Variscan Toledo Anatectic Complex, Central Iberia

open access: yes, 2016
In the Central Iberian Zone there are several large thermal domes in which small bodies of ultramafic, mafic and intermediate rocks appear intimately associated with crustal granites and migmatites.
J.F. Molina (2845070)   +7 more
core   +1 more source

Formation of kyanite-bearing migmatites in the Central Adirondacks

open access: yes, 2017
Sillimanite-rich, S-type, granitic migmatites exposed at Ledge Mountain represent the only location in the Adirondack Highlands where kyanite has been found. The texturally young kyanite overprints sillimanite in largely undeformed pegmatitic leucosomes,
Jackson Vincent Reeder
core  

Recumbent folding in migmatites in the Archean "basement" north of Nathdwara, Rajasthan, India

open access: yes, 1962
Structural studies of the migmatites, calc-granulites, and para-amphibolite inclusions of the banded gneiss complex in the vicinity of Nathdwara show the region to be tectonically homogeneous.
K. Naha   +3 more
core   +1 more source

The orthogneiss-derived migmatites of the Variscan Ulten Zone, Northeastern Italy: limited magma movement through the lower crust

open access: yes, 2011
Anatectic melt (or magma) created in migmatites, is potentially mobile (Sawyer, 2008). The Variscan Ulten Zone, on the contrary, provides an example of limited melt transfer within a km-sized lower crust.
Langone A., BRAGA, ROBERTO, Mazza S.
core  

Episodic water-fluxed anatexis recorded by migmatites from the Paleozoic Wuyi-Yunkai Orogeny in South China

open access: yes
The Wuyi-Yunkai Orogeny (WYO) in South China occurred during the assembly of Gondwana, and has abundant granites and migmatites which have been mostly interpreted as products of dehydration anatexis.
Zhao, Jun-Hong   +15 more
core   +1 more source

Genesis of metapelitic migmatites in the Adirondack Mts., New York

open access: yes, 2009
Oxygen isotope ratios and rare earth element (REE) concentrations provide independent tests of competing models of injection v. anatexis for the origin of migmatites from amphibolite and granulite facies metasedimentary rocks of the Adirondack Mountains,
McLelland, J.M.   +7 more
core   +1 more source

Applications and limitations of thermobarometry in migmatites and granulites using as an example rocks of the Araçuaí Orogen in southern Bahia, including a discussion on the tectonic meaning of the current results

open access: yesBrazilian Journal of Geology
In southern Bahia, there are outcrops of migmatites and granulites in the Jequitinhonha Complex, which is part of the northern portion of the Araçuaí Orogen.
Renato Moraes   +4 more
doaj   +1 more source

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