granulite वाक्य
उदाहरण वाक्य
मोबाइल
- The metamorphic transition from mafic granulite facies to the denser eclogite facies in the lower portion of the crust is the main mechanism responsible for creating negative buoyancy of the lower lithosphere.
- Syenitic gneiss accounts for about 40 % covering the southern, western and north-eastern corner of the city and also in form of scattered small intrusions into the pyroxene granulite gneiss.
- Fluid inclusions trapped within granulite facies rocks have provided important clues on the petrogenesis of dry granulite facies rocks through the influx of CO 2-rich fluids from sub-lithospheric sources.
- Fluid inclusions trapped within granulite facies rocks have provided important clues on the petrogenesis of dry granulite facies rocks through the influx of CO 2-rich fluids from sub-lithospheric sources.
- Mesoproterozoic igneous protoliths ( metamorphosed to granulite facies during the orogeny ) fall into two age groups in Mexico; ca . 1235-1115 Ma and ca . 1035-1010 Ma.
- The metamorphic conditions which parallel the deformation increase from west to east and from middle amphibolite to granulite facies . metamorphic event, resulting from probable continental collision . ( Madore, 2001 ).
- The metamorphic grade increases gradually from the Prince Olav Coast ( amphibolite facies; eastern part of the LHC ) to the Soya Coast ( granulite facies; western part of the LHC ).
- The possibility that it represents the transition from amphibolite facies to granulite facies metamorphism has been given some support from observations of the uplifted central part of the Vredefort Dome and the surrounding Kaapvaal craton.
- The Ampanihy ductile shear zone was created by flattening events associated with granulite metamorphism, isoclinal folding, flattened sheaths, steep to vertical foliations and sheath-like geometry of massif-type anorthosite bodies.
- Hornblende granulite subfacies is a transitional coexistence region of anhydrous and hydrated ferromagnesian minerals, so the above-mentioned isograds mark the boundary with " pyroxene granulite subfacies " facies with completely anhydrous mineral assemblages.
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