Pyroxenes from lherzolite
inclusions of Itinome-gata, Japan.
Chaussidon and J.-P Lorand, "Sulphur isotope composition of orogenic spinel lherzolite
massifs from Ariege (North-Eastern Pyrenees, France): an ion microprobe study," Geochimica et Cosmochimica Acta, vol.
The basis of this proposal is to experimentally determine high pressure-temperature melting phase relations along two critical regions of the melting curve, plagioclase-spinel lherzolite
and spinel-garnet lherzolite
(2006): Trace element partitioning between mica-and amphibole-bearing garnet lherzolite
and hydrous basanitic melt: 1.
The peridotite unit rocks are the most altered part of Noorabad ophiolite including dunite, harzburgite and lherzolite
. These rocks can be seen form many large and small mass of green to gray.
The foliated peridotite sequence is harzburgite-type (Nicolas, 1989) although minor lherzolite
has also been reported from the basal section of the mantle sequence (Mahmood et al., 1995).
, harzburgite, dunite mantle xenoliths, and xenocrystic debris are common and abundant in the ankaratrites and nephelinites  from eastern ASV (Figure 3).
Melting of phlogopite-bearing peridotite produces potassic rather than sodic magmas, but melting of amphibole- and clinopyroxene-bearing lherzolite
yields magmas with low CaO/[Al.sub.2][O.sub.3], variable Mg#s, and [K.sub.2]O/[Na.sub.2]O <1, characteristic of enriched lavas of the NE Pacific.
The dominant rock-type of the Balmuccia peridotite massif is a medium- to coarse-grained, porphyroclastic spinel lherzolite
Diamonds are known to occur in three peridotite subtypes: dunite (90% olivine), harzburgite (40-90% olivine, the rest orthopyroxene and garnet), and lherzolite
(at least 40% olivine, with orthopyroxene and clinopyroxene in a wide range of proportions, and minor garnet).
The Precambrian Ophiolits in north of Anarak are seen underneath the Precambrian-lower Cambrian metamorphics  and are of Harzburgite and partly lherzolite
accompanied with whom scattered masses of gabbro, Diabase, and plagiogranite are observed.
These observations and isotopic characteristics of the lavas suggest that their magmas were probably derived from partial melting of a subduction-metasomatized continental lithospheric mantle in the garnet/spinel lherzolite