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

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

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

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

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

FE-MG M1 SITE DISTRIBUTION IN SOME CLINOPYROXENES FROM SANTA OLALLA (HUELVA, SPAIN) = REPARTITION DES SITES M1 FE-MG DANS QUELQUES CLINOPYROXENES DE SANTA OLALLA (HUELVA, ESPAGNE)ARRIORTUA MI; AMIGO JM; DECLERCQ JP et al.1981; ACTA GEOL. HISP.; ISSN 0567-7505; ESP; DA. 1981; VOL. 16; NO 4; PP. 189-190; BIBL. 9 REF.; 4 TAB. ; TABL./ILL.Article

VNUTRIKRISTALLICHESKOE RASPREDELENIE KATIONOV FE³⁺ AL V KLINOPIROKSENE CAFE³⁺ALSIO₆ = REPARTITION DES CATIONS FE³⁺ ET AL DANS LE CRISTAL DU CLINOPYROXENE CAFE³⁺ALSIO₆KUREPIN VA; POL'SHIN EH V; ALIBEKOV GI et al.1981; MINERAL. ZH.; ISSN 0204-3548; SUN; DA. 1981; VOL. 3; NO 1; PP. 83-88; ABS. ENG; BIBL. 8 REF.; 1 TAB. ; TABL./ILL.Article

ELECTRON PETROGRAPHY OF EXSOLUTION TEXTURES IN AN IRON-RICH CLINOPYROXENE.COPLEY PA; CHAMPNESS PE; LORIMER GW et al.1974; J. PETROL.; G.B.; 1974, VOL. 15, NUM. 0001, P. 41 A 57Serial Issue

La précipitation discontinue omphacite=clinopyroxène+plagioclase: contribution à l'étude de l'évolution thermique des éclogites = The discontinuous precipitation omphacite→clinopyroxène+plagioclase: contribution to the eclogites thermal evolutionJoanny, Véronique; Lardeaux, Jean-Marc; Boudeulle, Micheline et al.1991, 137 p.Thesis

Primary relationships between CPX-gabbros and Fe-gabbros near Fetovaia, Elba Island, Italy = Les relations primaires entre gabbros à CPX et gabbros à Fe près de Fetovaia, île d'ElbeBORTOLOTTI, V; PICCARDO, G. B; PRINCIPI, G et al.1984, Vol 9, Num 1, pp 89-92, issn 0391-2612Article

Opticheskie spektry pogloshcheniya vanadisoderzhashchego diopsida―lavrovitaPLATONOV, A. N; KHOMENKO, V. M; BELICHENKO, V. P et al.Zapiski Vsesoûznogo mineralogičeskogo obŝestva. 1984, Num 6, pp 724-727, issn 0044-1805Article

Termodinamika i geotermometriya dvupiroksenogo ravnovesiyaSLAVINSKIJ, V. V.Doklady Akademii nauk SSSR. 1983, Vol 271, Num 4, pp 948-951, issn 0002-3264Article