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Wehrlite from
La Grille volcano, Grand Comore, Comoros


Locality type:Volcano
Classification
Type:Wehrlite
Confirmation
Validity:Believed Valid
Data
Mineral Data:Click here to view Wehrlite data
Locality Data:Click here to view La Grille volcano, Grand Comore, Comoros
Data Identifiers
Mindat Occurrence Record ID:1419270
Long-form Identifier:1:3:1419270:6
GUID (UUID V4):0
References
Reference Search (possible matching items)
Journal (article/letter/editorial)
Clinopyroxenes and Glasses in Ultramafic Xenoliths of Grande Comore, Indian Ocean M. COLTORTI1∗, C. BONADIMAN1, R....xenoliths (lherzolites and wehrlites) from La Grille volcano, Grande Comore island. These xenoliths have peculiar...respect, the peridotite xenoliths from La Grille volcano (Grande Comore island) are of primary importance...beneath Grande Comore was a carbonate-rich melt. Mineral and glass compositions of the La Grille xenoliths...volcanic islands; Grande Comore, Moheli, Anjouan and Mayotte (Fig. 1). Grande Comore, the westernmost and
Journal (article/letter/editorial)
The Petrology of the Lavas of Grande Comore by D. F. STRONG Department of Geology, Memorial University...islands are Mayotte, Anjouan, Moheli, and Grande Comore, distributed over a distance of 275 km along a...the east to the two active volcanoes of Grande Comore in the west. [Journal of Petrology, Vol. 13, P«rt...submerged Mayotte to the active Kartala volcano on Grande Comore. The volcanic rocks on all the islands...derivatives. Grande Comore is formed of two coalescing shield volcanoes, La Grille in the north and Kartala
Journal (article/letter/editorial)
plume–lithosphere interactions in the genesis of Grande Comore magmas žIndian Ocean / C. Deniel ) UMR 6524 CNRS...distinguished among the Grande Comore lavas: Old Karthala, Recent Karthala and La Grille. Major and trace element...slightly undersaturated lavas Žshield-stage. and La Grille strongly undersaturated primary melts Žpost-shield...incompatible elements, with relative enrichments in Ba, Nb, La and relative depletions in Rb, K, Sr, Sm. Low HREE...indicate that garnet is residual in their sources. La Grille lavas exhibit the highest and most variable degrees
Book (volume)
Oceanography La Jolla, California David K. Hobday Joseph R. Curray Scripps Institution of Oceanography La Jolla...Lumpur, Malaysia Scripps Institution of Oceanography La Jolla, California P. E. Kent Natural Environment...David G. Moore Scripps Institution of Oceanography La Jolla, California Alan E. M. Nairn Department of...I.M 200' ::: _:::. I!Oc .~~~~. 300' ~~~~~ -.-la~ .00- ~:~~~ 110.... 01' ~ .:-:~ . INNER FAN ...Clocchiatti, M., 1976, La dissolution des carbonates en milieu oceanique. Son role dans la genese des depots
Book
Er Eu F Fe Fr Ga Gd Ge H He Hf Hg Ho I In Ir Κ Kr La Li Lu Mg Mn dysprosium erbium europium fluorine...1.1 MINERALOGY OF IGNEOUS ROCKS 3 (continued) La Ce Pr Nd [Pm] Sm Eu Gd Tb Dy Ho Er Tm Yb Lu Lanthanum...1.81 1.96 1.32 1.25 1.72 1.72 1.34 Sc 3+ Y 3+ La 3+ Ce 2+ Eu 3+ Eu 3+ Lu 2+ Sr 2+ Ba + K + Rb +...H ) 2 Α , Β, C, F, G, Ν, Ρ a, c Monazite (Ce,La,Th)P04 G, Ρ Fluorite CaF2 Ρ f Calcite CaC03...may be superimposed to form a basaltic shield volcano with low-angle slopes commonly no steeper than
 
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