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Microtectures of lunar and meteoritic clinopyroxenes as petrological indicators = Microtextures des clinopyroxènes lunaires et météoritiques comme indicateurs pétrologiquesKHISINA, N. R.Mezhdunarodnyj geologicheskij kongress. 27. 1984, pp 309-311Conference Paper

CLINOENSTATITE AS AN EXSOLUTION PHASE IN DIOPSIDE.YAMAGUCHI Y; TOMITA K.sdMEM. FAC. SCI., KYOTO UNIV., GEOL. MINERAL.; JPN; , P. 173 A 180Miscellaneous

THE CORRELATION BETWEEN THE SI-O (BRIDGING) DISTANCE AND THE FREQUENCY OF THE SI-O-SI STRETCHING IN CLINOPYROXENES = CORRELATION ENTRE LA DISTANCE SI-O (PONTANT) ET LA FREQUENCE DE L'ALLONGEMENT DE SI-O-SI DANS LES CLINOPYROXENESOHASHI H; OSAWA T.1981; GANSEKI KOBUTSU KOSHO GAKKAISHI; ISSN 0021-4825; JPN; DA. 1981; VOL. 76; NO 5; PP. 172-175; ABS. JAP; BIBL. 17 REF.; 1 TAB. ; ILL./TABL.Article

GROWTH HABITS OF CLINOPYROXENE.FLEET ME.1975; CANAD. MINERALOGIST; CANADA; DA. 1975; VOL. 13; NO 4; PP. 336-341; ABS. FR.; BIBL. 20 REF.; 3 ILL.Article

DISTORSIONS IN THE COORDINATION POLYHEDRA OF M SITE ATOMS IN OLIVINES, CLINOPYROXENES, AND AMPHIBOLES.FLEET ME.1974; AMER. MINERALOGIST; U.S.A.; DA. 1974; VOL. 59; NO 9-10; PP. 1083-1093; BIBL. 1 P.; 9 ILL.Article

IMMISCIBILITY OF THE NATURAL PYROXENES DIOPSIDE AND FASSAITE AND THE CRITERION FOR IT.GINZBURG IV.1969; DOKL. EARTH SCI. SECT.; USA; 1969(4), VOL. 186, P. 106 A 109Miscellaneous

CRYSTAL STRUCTURES OF CA-RICH CLINOPYROXENES ON THE CAMGSI2O6-MG2SI2O6 JOIN = STRUCTURES CRISTALLINES DES CLINOPYROXENES RICHES EN CA DE LA SERIE CAMGSI2O6-MG2SI2O6BRUNO E; CARBONIN S; MOLIN G et al.1982; TMPM, TSCHERMAKS MINERAL. PETROGR. MITT.; ISSN 0041-3763; AUT; DA. 1982; VOL. 29; NO 4; PP. 223-240; ABS. ENG; BIBL. 2 P.; 6 TAB. ; TABL./ILL.Article

Moyens actuels d'identification de la JADEITE verte = Contemporary identification to green JADEITEMOK, D.Revue de gemmologie A.F.G. 1999, Num 136, pp 11-13, issn 0398-9011Article

A new schemes for calculating mineral end members with reference to clinopyroxene and garnetYANG JIANJUNNGSE.Dìzhìxué bào. 1991, Vol 65, Num 4, pp 359-366, issn 0001-5717Article

Une nouvelle méthode pour mesurer les angles d'extinction maximum du clinopyroxène et de l'amphibole au microscope polarisantFU DEBIN.Dìzhì lùmpíng. 1987, Vol 33, Num 1, pp 29-39, issn 0371-5736Article

A volcanic inclusions based approach for provenance studies of archaeological ceramics: application to pottery from southern ItalyBARONE, Germana; BELFIORE, Cristina Maria; MAZZOLENI, Paolo et al.Journal of archaeological science. 2010, Vol 37, Num 4, pp 713-726, issn 0305-4403, 14 p.Article

The second Liesegang-layered clinopyroxene megacryst inclusion from Szentbékalla, Balaton-Highlands, HungaryBERCZI, S; TOROK, K.International geological congress. 1992, p.706Conference Paper

Ca-Sr substitution in clinopyroxenes along the join CaMgSi2O6-SrMgSiO6 = La substitution Ca-Sr dans les clinopyroxènes le long de l'interface CaMgSi2O6-SrMgSi2O6BENNA, P.TMPM. Tschermaks mineralogische und petrographische Mitteilungen. 1982, Vol 30, Num 1, pp 37-46, issn 0041-3763Article

Clinopyroxenes ans spinels in the system CaMgSi2O6-CaAl2SiO6-CaGrAlSiO6: a preliminary report = Clinopyroxènes et spinelles dans le système CaMgSi2O6-CaAl2SiO6-CaCrAlSiO6: rapport préliminaireONUMA, K; TOHARA, T.Journal of the Faculty of Science. Hokkaido University, Series 4 : Geology and Mineralogy. 1981, Vol 19, Num 4, pp 495-503, issn 0018-3474Article

Triple chain structure slabs nucleated in Cpx from submarine rock specimens and their slab formation mechanismAKAI, J; KOMATSU, M.International geological congress. 1992, p.684Conference Paper

Ti- and Al-rich clinopyroxenes from the dolerite dike in the Meguro area of the Hidaka metamorphic belt, Hokkaido = Clinopyroxènes riches en titane et aluminium du dyke doléritique de la région Meguro, zone métamorphique Hidaka, HokkaïdoMAEDA, J.Journal of the Faculty of Science. Hokkaido University, Series 4 : Geology and Mineralogy. 1981, Vol 20, Num 1, pp 79-86, issn 0018-3474Article

Détermination des orientations préférentielles de réseau de l'omphacite : les avantages del'EBSD = Determination of preferred orientations in the lattice of omphacite : the advantages of EBSDMAULER, A; KUNZE, K; BURG, J. P et al.Réunion des Sciences de la Terre. 1998, p. 159Conference Paper

NEKOTORYE KRISTALLOKHIMICHESKIE ASPEKTY PLEOKHROIZMA ZHELEZOSODERZHASHCHIKH KLINOPIROKSENOV = QUELQUES ASPECTS CRISTALLOCHIMIQUES DU PLEOCHROISME DE CLINOPYROXENES CONTENANT DU FERKHOMENKO VM; PLATONOV AN.1982; MINERAL. ZH.; ISSN 546895; UKR; DA. 1982; NO 4; PP. 38-45; ABS. ENG; BIBL. 15 REF.; 4 TAB. ; TABL./ILL.Article

PARTICULARITES DE LA METASOMATOSE EN RELATION AVEC LA GENESE DU MAGMATISME BASIQUE NON PROFONDPAVLOV AL; REVERDATTO VV.1972; ZAP. VSESOJUZ. MINERAL. OBSHCHEST.; S.S.S.R. ; 1972, VOL. 101, NUM. 0004, P. 413 A 420Serial Issue

DIFFRACTOGRAMMES RX ET SPECTRES D'ABSORPTION IR D'AUGITES FERRIFERES.RASHIN GA; LEBEDEVA GA; BUGNIN GA et al.1971; INST. GEOL., TRUDY, LENINGRAD; SUN; 1971, VOL. 7, P. 173 A 177Miscellaneous

FERROAN SAHLITE FROM THE EASTERN GHATS, ANDHRA PRADESH, INDIA.RAO AT; RAO KSR.1971; MINERAL. MAG.; GBR; 1971, VOL. 38, NUM. 0295, P. 377 A 379Miscellaneous

Dvupiroksenaya geotermometriyaSLAVINSKIJ, V. V.1983, Vol 5, Num 6, pp 29-38Article

The M2S projection int CS-MS-A: a comparison of Na2O and FeO bearing systems = La projection de M2S dans le plan CS-MS-A comparaison des systèmes contenant Na2O et FeOBIGGAR, G. M; HUMPHRIES, D. J.1981, Num 5, issn 0309-6882, 161Article

Mikrostrukturnye osobennosti Klinopiroksenov iz ehklogitov i ehklogitopodobnykh porodSTENINA, N. G; SHATSKIJ, V. S.Mezhdunarodnyj geologicheskij kongress. 27. 1984, 179Conference Paper

Cristallochimica di clinopirosseni ricchi in Ca di senie vulcaniche alcaline e «transizionali» = Cristallochimie des pyroxènes monocliniques riches en Ca de séries volcaniques alcalines et «transitionnelles»CARBONIN, S; MOLIN, G. M; MUNNO, R et al.Rendiconti della Societa Italiana di Mineralogia e Petrologia. 1982, Vol 38, Num 2, issn 0037-8828, 901Article

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