Skip Nav Destination
Article navigation
Other|
January 01, 1990
Growth defects and growth marks in pegmatite beryls
E. Scandale;
E. Scandale
Univ. Bari, Dip. Geomineral., I-70124 Bari, Italy
Search for other works by this author on:
E. Scandale
Univ. Bari, Dip. Geomineral., I-70124 Bari, Italy
S. Lucchesi
G. Graziani
Publisher: Deutsche Mineralogische Gesellschaft, Sociedad Española de Mineralogia, Societá Italiana di Mineralogia e Petrologia, Société Francaise de Minéralogie
First Online:
02 Mar 2017
Online Issn: 1617-4011
Print Issn: 0935-1221
GeoRef, Copyright 2004, American Geological Institute. Reference includes data from Geoline, Bundesanstalt fur Geowissenschaften und Rohstoffe, Hanover, Germany
European Journal of Mineralogy (1990) 2 (3): 305–311.
Article history
First Online:
02 Mar 2017
Citation
E. Scandale, S. Lucchesi, G. Graziani; Growth defects and growth marks in pegmatite beryls. European Journal of Mineralogy 1990;; 2 (3): 305–311. doi:
Download citation file:
You could not be signed in. Please check your email address / username and password and try again.
Index Terms/Descriptors
Latitude & Longitude
Citing articles via
Related Articles
BERYL FROM MIAROLITIC POCKETS OF GRANITIC PEGMATITES, ELBA, ITALY: CHARACTERIZATION OF CRYSTAL CHEMISTRY BY MEANS OF EMP AND SIMS ANALYSES
The Canadian Mineralogist
IRON+MAGNESIUM-BEARING BERYL FROM GRANITIC PEGMATITES: AN EMPA, LA-ICP-MS, MÖSSBAUER SPECTROSCOPY, AND POWDER XRD STUDY
The Canadian Mineralogist
Cs-bearing Beryl Evolving To Pezzottaite from the Julianna Pegmatitic System, Sw Poland
The Canadian Mineralogist
Mn-tourmaline crystals from island of Elba (Italy): Growth history and growth marks
American Mineralogist
Related Book Content
Beach sands of Elba Island, Tuscany, Italy: Roundness study and evidence of provenance
Processes Controlling the Composition of Clastic Sediments
Rare-Element Granitic Pegmatites
Rare Earth and Critical Elements in Ore Deposits
Surface chemistry of oil-sands clay minerals
Introduction to Oil Sands Clays
Inorganic geochemistry of domed peat in Indonesia and its implication for the origin of mineral matter in coal
Modern and Ancient Coal-Forming Environments