A Petrographic Atlas of Ophiolite
An example from the eastern India-Asia collision zone
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Reverse fractionation modeling considering energy-constrained assimilation-fractional crystallization is performed to estimate primary magma compositions, degree of crustal contamination, pressure–temperature ...
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Strongly SiO2-undersaturated alkalic rocks (Mg# > 50, SiO2 ≤ 45 wt%, Na2O + K2O ≥ 3 wt%) occur in three early-stage (Sarnu-Dandali, Mundwara, Bhuj) and one late-stage (Murud-Janjira) rift-associated volcanic comp...
Article
The Powai ankaramite flow from Mumbai, western Deccan Traps, contains abundant crystals of augite (En59–47Fs10–14Wo27–42, 22–40 modal %, 3–5 mm) and olivine (Fo84–74, 11–16 modal %, 1–2 mm), and minor plagioclase...
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Ultrahigh-pressure (UHP) rocks such as the coesite-bearing eclogites, occurring as boudins within felsic gneisses of the Tso Morari dome in northwestern Himalayas, originated through subduction of the northern...
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Plate Chr-1: Brecciated olivine with euhedral chromite and a vein of serpentine containing granular opaque magnetite in harzburgite tectonite. (380/79-3)
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Greenschist consisting of actinolite, chlorite, albite, epidote and quartz. The amphiboles impart lineation(23/80-1)
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Plate Nimi-1 Elongated tabular crystals of staurolite and muscovite flakes along foliation in chlorite-biotite-muscovite-garnet-staurolite schist with quartz and feldspar from the Nimi Formation at the eastern...
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Plate Pc-1 Small grains of olivine remnants and opaque in serpentinised dunite. The olivine grains show uniform extinction indicating absence of strain (126/80-2)
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Plate PG-1: Hypidiomorphic granular texture in tonalite between crossed polars consisting of twinned plagioclase, quartz, amphibole, chlorite and epidote. Chlorite is more abundant than amphibole (M-1-3).
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Plate Vlgm-1: Very-low grade, zeolite facies metamorphite between crossed polars containing spherulitic natrolite, twinned albite, epidote, green chlorite and opaque. (K-79-7)
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Plate Ltg-1 Late felsic intrusive under crossed polars showing post-crystalline deformation with parallel orientation of quartz and feldspar grains. Plagioclase is saussuritised and twinned. K-feld...
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The evolution of the NHO is linked with the fragmentation and dispersion of Gondwana (protocontinent of the southern hemisphere) and its subsequent collision and amalgamation with Eurasia during Meso-Cenozoic ...
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The average composition of peridotite from the ophiolite belt in Manipur shows high MgO(32.0 wt.%), Al2O3 (1.28–3.30 wt.%),Ni (1966 ppm),Cr (2005 ppm)and Co (130 ppm) and low TiO2 (0.12 wt.%), CaO (6.56 wt.%), Na