SILICA DISSOLUTION AND OVERGROWTH OF FOSSIL DIATOMS = DISSOLUTION ET SURCROISSANCE DE LA SILICE CHEZ LES DIATOMEES FOSSILESMIKKELSEN N.1977; MICROPALEONTOLOGY; ISSN 0026-2803; USA; DA. 1977; VOL. 23; NO 2; PP. 223-226; BIBL. 19 REF.Article

OVERGROWTH COMPETITION BETWEEN ENCRUSTING CHEILOSTOME ECTOPROCTS IN A JAMAICAN CRYPTIC REEF ENVIRONMENTJACKSON JBC.1979; J. ANIMAL ECOL.; GBR; DA. 1979; VOL. 48; NO 3; PP. 805-823; BIBL. 2 P.Article

MANTLED FELDSPARS AND SYNNEUSISSTULL RJ.1979; AMER. MINERALOGIST; USA; DA. 1979; VOL. 64; NO 5-6; PP. 514-518; BIBL. 22 REF.; 5 ILL.Article

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U-PB ISOTOPE ANALYSES OF ZIRCONS FROM A PRECAMBRIAN GNEISS AREA IN NORTHEASTERN SWEDEN AND THEIR CHRONOSTRATIGRAPHIC IMPLICATIONS = ANALYSES ISOTOPIQUES U-PB DE ZIRCONS D'UNE ZONE DE GNEISS PRECAMBRIENS DANS LE NE DE LA SUEDE ET LEURS IMPLICATIONS CHRONOSTRATIGRAPHIQUESSKIOELD T.1981; ABST. GEOCHRONOL. ISOT. GEOL.; ISSN 0304-5935; BEL; DA. 1981; NO 38; 1 P.Article

IRON FORMATION OF PRECAMBRIAN AGE: HEMATITE-MAGNETITE RELATIONSHIPS IN SOME PROTEROZOIC IRON DEPOSITS - A MICROSCOPIC OBSERVATION = FORMATIONS FERRIFERES D'AGE PRECAMBRIEN: LES RAPPORTS HEMATITE-MAGNETITE DANS QUELQUES GITES DE FER PROTEROZOIQUES. OBSERVATIONS MICROSCOPIQUESHAN TM.1982; ORE GENESIS. THE STATE OF THE ART; DEU; BERLIN: SPRINGER; DA. 1982; PP. 451-459; BIBL. 7 REF.; ISBN 3-540-11139-5; ILL.Book Chapter

EFFECT OF FAULT-RELATED GRANULATION ON POROSITY AND PERMEABILITY OF QUARTZ SANDSTONES, SIMPSON GROUP (ORDOVICIAN), OKLAHOMA = L'EFFET DE LA GRANULATION LIEE AUX FAILLES SUR LA POROSITE ET LA PERMEABILITE DES GRES QUARTZEUX, GROUPE SIMPSON (ORDOVICIEN) OKLAHOMAPITTMAN EDWARD D.1981; AAPG BULL.; ISSN 0149-1423; USA; DA. 1981-11; VOL. 65; NO 11; PP. 2381-2387; BIBL. 15 REF.; ILL.Article

DIAGENESIS OF NUBIA SANDSTONE AS REVEALED BY SCANNING ELECTRON MICROSCOPY = LA DIAGENESE DES GRES DE NUBIE REVELEE PAR L'OBSERVATION AU MICROSCOPE A BALAYAGE ELECTRONIQUEEZZELDIN HILMY M; HUSSEIN SA.1978; EGYPT. J. GEOL.; EGY; DA. 1978; VOL. 22; NO 2; PP. 87-101; ABS. ARA; BIBL. 3 P.; 5 PLANCH. ; PL.Article

FORMATION OF QUARTZ OVERGROWTHS IN THE NUBIA SANDSTONE OF KHARGA OASIS (WESTERN DESERT, EGYPT) AS REVEALED BY SCANNING ELECTRON MICROSCOPY = FORMATION DE QUARTZ A BORDURES EPITAXIQUES DANS LE GRES DE NUBIE DE L'OASIS DE KHARGA, DESERT OCCIDENTAL D'EGYPTE TELLE QUE LA MONTRE LA MICROSCOPIE ELECTRONIQUE PAR BALAYAGEABU ZEID MM.1982; NEUES JAHRB. MINERAL., ABH.; ISSN 0077-7757; DEU; DA. 1982; VOL. 143; NO 2; PP. 122-140; BIBL. 33 REF.; ESQUISSE/ILL.Article

CROISSANCE CRISTALLINE DES MINERAUX. APPORTS RECENTS ET PERSPECTIVES DE LA MICROSCOPIE ELECTRONIQUE EN TRANSMISSIONBARONNET A.1982; J. MICROSC. SPECTROSC. ELECTRON.; ISSN 0395-9279; FRA; DA. 1982; VOL. 7; NO 4; PP. 417-423; BIBL. 34 REF.Conference Paper

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DOWNWARD DEVELOPMENT OF OVERGROWTHS FROM ECHINODERM FRAGMENTS IN A SUBMARINE ENVIRONMENTNACI GORUR.1979; SEDIMENTOLOGY; NLD; DA. 1979; VOL. 26; NO 4; PP. 605-608; BIBL. 13 REF.; 2 ILL.Article

Calcite and aragonite precipitation from seawater solutions of various salinities : precipitation rates and overgrowth compositions = Précipitation de calcite et d'aragonite à partir de solutions d'eau de mer de différentes salinités. Taux de précipitation et compositions des minéraux produits par surcroissanceSHAOJUN ZHONG; MUCCI, A.Chemical geology. 1989, Vol 78, Num 3-4, pp 283-299, issn 0009-2541Conference Paper

Structure refinement and genetic aspects of a microcline overgrowth on amazonite from Pikes Peak batholith, Colorado, USA = Affinement de la structure et aspects génétiques d'une surcroissance de microcline sur amazonite, provenant du batholite Pikes Peak, Colorado, Etats-UnisBLASI, A; BRAJKOVIC, A; DE POL BLASI, C et al.Bulletin de minéralogie. 1984, Vol 107, Num 3-4, pp 411-422, issn 0180-9210Article

Pb—Pb zircon ages of Archaean metasediments and gneisses from the Dharwar craton, southern India: Implications for the antiquity of the eastern Dharwar cratonMAIBAM, B; GOSWAMI, J. N; SRINIVASAN, R et al.Journal of earth system science (Print). 2011, Vol 120, Num 4, pp 643-661, issn 2347-4327, 19 p.Article

Syntaxial overgrowth in muddy crinoidal limestones: cathodoluminescence sheds new light on an old problem = Surcroissance par syntaxie dans des calcaires à crinoïdes: la cathodoluminescence apporte un nouveau point de vue sur un problème ancienWALKDEN, G. M; BERRY, J. R.Sedimentology. 1984, Vol 31, Num 2, pp 251-267, issn 0037-0746Article

Determination of pressure solution shortening in sandstonesONASCH, C. M.Tectonophysics. 1993, Vol 227, Num 1-4, pp 145-159, issn 0040-1951Article

O tsirkonijsoderzhashchikh narostakh na tsirkone iz pegmatitovMETS, O.F; POLEZHAEVA, L.I; MEN'SHIKOV, YU.P et al.Zapiski Vsesoûznogo mineralogičeskogo obŝestva. 1989, Vol 118, Num 4, pp 74-80, issn 0044-1805Article

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

The first fossil entoproctTODD, J. A; TAYLOR, P. D.Naturwissenschaften. 1992, Vol 79, Num 7, pp 311-314, issn 0028-1042Conference Paper

Surface planarity and microstructure of low temperature silicon SEG and ELOARST, M. C; RITZ, K. N; REDKAR, S et al.Journal of materials research. 1991, Vol 6, Num 4, pp 784-791, issn 0884-2914Article

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Porosity reduction in sandstone by quartz overgrowthLEDER, F; PARK, W. C.AAPG bulletin. 1986, Vol 70, Num 11, pp 1713-1728, issn 0149-1423Article

Oriented overgrowth of acicular maghemite-crystals on quartz = Surcroissance orientée de cristaux aciculaires de maghémite sur du quartzABREU, M. M; FIGUEIREDO, M. O; WAERENBORGH, J. C et al.Clay minerals. 1988, Vol 23, Num 4, pp 357-365, issn 0009-8558Conference Paper