dunite वाक्य
उदाहरण वाक्य
मोबाइल
- The mountain consists mostly of soapstone and dunite.
- Rock types include picrite, peridotite, dunite, pyroxenite, gabbro and granophyre.
- Samples of the ridge from the Afanasy Nikitin Seamount were ultramafic dunite . hotspot.
- Dunite xenoliths are found within the erupted basalts.
- Olivine and dunite, both found in subducted crust, are materials of this sort.
- Low silicon content is indicative of mafic and ultramafic igneous rocks, such as basalt and dunite.
- The parent rock of this banded variety most likely was a pyroxenite enclosing cumulate layers of dunite.
- Peridotite and dunite, when fresh, can contain up to ~ 4, 000 ppm nickel within olivine.
- Amphibolite and chert tectonic blocks also occur in the dunite near the area's southern and western boundaries.
- The Lherz massif also contains harzburgite and dunite, as well as layers of spinel pyroxenite, garnet pyroxenite, and hornblendite.
- In southern British Columbia, Canada dunite rocks form the core of an ultramafic rock complex located near the small community of Tulameen.
- Hellyerite forms in this environment in nickel rich serpentinites, which are metamorphosed equivalents of ultramafic cumulate rocks such as peridotite and dunite.
- This is an area of serpentine soil derived from olivine and dunite that prevent forest growth, and is instead naturally barrens and savannas.
- The fern thrives in thin serpentine soils on sunny, disturbed habitats such as roadcuts and talus slopes, in dunite and other ultramafic rocks.
- Green sand for aluminum typically uses olivine sand ( a mixture of the minerals forsterite and fayalite, which is made by crushing dunite rock ).
- "' Heazlewoodite "', Ni 3 S 2, is a rare sulfur-poor nickel sulfide mineral found in serpentinitized dunite.
- Other geologic features of the area include northeastward trending dikes that consists of massive, dark brown, hornblende-plagioclase diorite which intruded into the dunite bedrock.
- Primary or orthomagmatic chromites are sporadically distributed in the ultramafics although major economic deposits are generally concentrated in the transition zone between residual harzburgite and cumulate dunite unit.
- Ultramafic rocks such as peridotite and dunite can be residues left after extraction of magmas, and typically they are more enriched in olivine after extraction of partial melts.
- The dunite intruded into andesite pillow breccias and flows of the Pe�on Blanco volcanic formation, which crops out near the northeast and southern boundaries of the Management Area.
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