Stability of high-density clinoenstatite at upper-mantle pressuresANGEL, R. J; CHOPELAS, A; ROSS, N. L et al.Nature (London). 1992, Vol 358, Num 6384, pp 322-324, issn 0028-0836Article

High temperature crystal structure refinements of low-clinoenstatite up to 700°C = Affinement de la structure cristalline à haute température de la clinoenstatite basse température jusqu'à 700°CPANNHORST, W.Neues Jahrbuch für Mineralogie. Abhandlungen. 1984, Vol 150, Num 3, pp 219-228, issn 0077-7757Article

Ortho/clinoenstatite transitionKANZAKI, Masami.Physics and chemistry of minerals. 1991, Vol 17, Num 8, pp 726-730, issn 0342-1791Conference Paper

ANALYTICAL ELECTRON MICROSCOPY IN MINERALOGY; EXSOLVED PHASES IN PYROXENES = MICROSCOPIE ELECTRONIQUE ANALYTIQUE EN MINERALOGIE: PHASES D'EXSOLUTION DANS LES PYROXENESNORD GL JR.1982; ULTRAMICROSCOPY; ISSN 0304-3991; NLD; DA. 1982; VOL. 8; NO 1-2; PP. 109-119; BIBL. 41 REF.; ILL.Conference Paper

Phase transition in Ca-poor clinopyroxes. A high temperature transmission electron microscopic studySHIMOBAYASHI, Norimasa; KITAMURA, Masao.Physics and chemistry of minerals. 1991, Vol 18, Num 3, pp 153-160, issn 0342-1791Conference Paper

Polysynthetically-twinned structures of enstatite and wollastonite = Macles polysynthétiques de l'enstatite et de la wollastoniteOHASHI, Y.Physics and chemistry of minerals. 1984, Vol 10, Num 5, pp 217-229, issn 0342-1791Article

EQUILIBRIA IN THE MG-RICH PART OF THE PYROXENE QUADRILATERAL = EQUILIBRE DE LA PARTIE RICHE EN MAGNESIUM DU QUADRILATERE PYROXENEJENNER GA; GREEN DH.1983; MINERALOGICAL MAGAZINE; ISSN 0026-461X; GBR; DA. 1983; VOL. 47; NO 2; PP. 153-160; BIBL. 24 REF.; TABL./ILL./ANAL.Article

STRUCTURE AND CRYSTAL CHEMISTRY OF PEROVSKITE-TYPE MGSIO₃.YAGI T; MAO HK; BELL PM et al.1978; PHYS. CHEM. MINER.; DEU; DA. 1978; VOL. 3; NO 2; PP. 97-110; BIBL. 2 P.; 9 ILL.Article

Computer simulation of the MgSiO3 polymorphsMATSUI, Masanori; PRICE, Geoffrey D.Physics and chemistry of minerals. 1992, Vol 18, Num 6, pp 365-372, issn 0342-1791Conference Paper

Fe-Mg heterogeneity in the low-Ca pyroxenes during metamorphism of the ordinary chondrites = Hétérogénéité Fe-Mg dans les pyroxènes faiblement calciques durant le métamorphisme des chondrites ordinairesTSUCHIYAMA, A; FUJITA, T; MORIMOTO, N et al.Symposium on antarctic meteorites. 12. 1988, pp 173-184Conference Paper

Solid-state oxygen 17 nuclear magnetic resonance spectroscopic studies of alkaline earth metasilicates = Etude spectroscopique RMN ¹⁷O à l'état solide de métasilicates de terre alcalineKYUNG, H; TIMKEN, C; SCHRAMM, S. E et al.Journal of physical chemistry (1952). 1987, Vol 91, Num 5, pp 1054-1058, issn 0022-3654Article

EXPERIMENTAL DETERMINATION OF THE HEATS OF FORMATION OF FORSTERITE AND CLINOENSTATITE = DETERMINATION EXPERIMENTALE DES CHALEURS DE FORMATION DE LA FORSTERITE ET DE LA CLINO-EUSTATITEKISELEVA IA; OGORODOVA LP; TOPOR ND et al.1981; MOSC. UNIV. GEOL. BULL.; ISSN 0145-8752; USA; DA. 1981; VOL. 36; NO 1; PP. 28-36; BIBL. 19 REF.; 8 TAB. ; ILL.Article

CLINOENSTATITE IN BONINITES FROM THE BONIN ISLANDS, JAPANSHIRAKI K; KURODA N; URANO H et al.1980; NATURE; GBR; DA. 1980; VOL. 285; NO 5759; PP. 31-32; BIBL. 16 REF.Article

THE THERMODYNAMIC EFFECT OF SHEAR STRESS ON THE ORTHO-CLINO INVERSION IN ENSTATITE AND OTHER COHERENT PHASE TRANSITIONS CHARACTERIZED BY A FINITE SIMPLE SHEAR.COE RS.1970; BEITR. MINERAL PETROL; DEU; 1970, VOL. 26, NUM. 0003, P. 247 A 264Miscellaneous

STABILITY RELATIONS OF SILICATE SPINELS, ILMENITES, AND PEROVSKITES = STABILITE DES SPINELLES, ILMENITES ET PEROVSKITES SILICATEESITO E; YAMADA H.1982; ADVANCES IN EARTH AND PLANETARY SCIENCES; ISSN 504696; JPN; DA. 1982; VOL. 12; PP. 405-419; BIBL. 16 REF.Article

THERMOCHEMISTRY OF SILICATE SOLID SOLUTIONS = THERMOCHIMIE DES SOLUTIONS SOLIDES DE SILICATESNEWTON RC; WOOD BJ; KLEPPA OJ et al.1981; BULL. MINERAL.; ISSN 0180-9210; FRA; DA. 1981; VOL. 104; NO 2-3; PP. 162-171; ABS. FRE; BIBL. 2 P.; TABL./ILL.Conference Paper

LE CALCUL DES TEMPERATURES D'EQUILIBRE DES ROCHES A MINERAIS DES GISEMENTS DE FE ET P DE FANSHAN, HEBEI ET LEUR IMPORTANCE GEOLOGIQUEJIANG PEIMO.1980; TUNG WU HSUEH PAO; ISSN 0001-7302; CHN; DA. 1980; VOL. 54; NO 4; PP. 275-283; ABS. ENG; BIBL. 3 REF.; 5 TAB. ; ILL./TABL.Article

PRINCIPAL STRESS DIRECTIONS FROM A NATURAL OCCURRENCE OF STRESS-INDUCED CLINOENSTATITEFROST BR; COE RS; OKAMURA FP et al.1978; CONTRIB. MINERAL. PETROL.; DEU; DA. 1978; VOL. 67; NO 2; PP. 119-126; BIBL. 24 REF.; 9 ILL.Article

LIAISON CHIMIQUE DANS LES SOLUTIONS SOLIDES DE DIOPSIDEVERESHCHAGIN VI; ROMANOV BP; KHISAMOV BA et al.1978; ZH. PRIKL. KHIM.; SUN; DA. 1978; VOL. 51; NO 9; PP. 2133-2134; BIBL. 10 REF.Article

High resolution transmission electron microscopic study of polytype in enstatiteYANGUO WANGG; WANKANG HUANG.International geological congress. 1992, p.695Conference Paper

CLINOENSTATITE IN VOLCANIC ROCK FROM THE BONIN ISLANDS = CLINOENSTATITE DANS UNE ROCHE VOLCANIQUE DES ILES BONINKOMATSU M.1980; CONTRIB. MINERAL. PETROL.; ISSN 0010-7999; DEU; DA. 1980; VOL. 74; NO 4; PP. 329-338; BIBL. 13 REF.; 43 ANAL.; 5 TAB. ; ILL./TABL./ANAL.Article

On the phase transformation proto- to clino/orthoenstatite: neutron powder investigationSCHRADER, H; BOYSEN, H; FREY, F et al.Physics and chemistry of minerals. 1990, Vol 17, Num 5, pp 409-415, issn 0342-1791Conference Paper

A transferable interatomic potential for crystalline phases in the system MgO-SiO2 = Potentiel interatomique transférable dans les phases cristallines du système MgO-SiO2LEINENWEBER, K; NAVROTSKY, A.Physics and chemistry of minerals. 1988, Vol 15, Num 6, pp 588-596, issn 0342-1791Article

Phase transition of orthoenstatite to high-clinoenstatite: in situ TEM study at high temperaturesSHIMOBAYASHI, N; KITAMURA, M.Mineralogical Journal. 1993, Vol 16, Num 8, pp 416-426, issn 0544-2540Article

Overgrowths textures, disequilibrium zoning, and cooling history of a glassy four-pyroxene boninite dyke from New CaledoniaOHNENSTETTER, D; BROWN, W.L.Journal of Petrology. 1992, Vol 33, Num 1, pp 231-271, issn 0022-3530Article