Article navigation
JOURNAL ARTICLE
Hydrated barium aluminosilicates, BaAl 2 Si 2 O 8 .n H 2 O, and their relations to cymrite and hexacelsian
Krishnamoorthy Viswanathan
Krishnamoorthy Viswanathan
Technische Universitaet, Institut fuer Geowissenschaften, Braunschweig, Federal Republic of Germany
Search for other works by this author on:
European Journal of Mineralogy (1992) 4 (2): 271-278.
Published:
April 01, 1992
Search
Search
Sign in
Don't already have an account? Register
You could not be signed in. Please check your email address / username and password and try again.
Index Terms/Descriptors
Citing articles via
Related Articles
P – Goldschmidt Abstracts 2013
Mineralogical Magazine
Ba minerals in clinopyroxene rocks from the Myanmar jadeitite area: implications for Ba recycling in subduction zones
European Journal of Mineralogy
M – Goldschmidt Abstracts 2013
Mineralogical Magazine
Na-Ba and K-Ba partitioning between feldspar and aqueous chloride solutions; some consequences of unmixing in solids and fluids
European Journal of Mineralogy
V – Goldschmidt Abstracts 2013
Mineralogical Magazine
Related Book Content
Microstructures of melt-bearing regional metamorphic rocks
Origin and Evolution of Precambrian High-Grade Gneiss Terranes, with Special Emphasis on the Limpopo Complex of Southern Africa
The White Mountain Granitoid Suite: Isotopic constraints on source reservoirs for Cretaceous magmatism within the Wrangellia Terrane
Tectonic Growth of a Collisional Continental Margin: Crustal Evolution of Southern Alaska
Uplift of the southeastern Australian lithosphere: Thermal-tectonic evolution of garnet pyroxenite xenoliths from western Victoria
The Crust-Mantle and Lithosphere-Asthenosphere Boundaries: Insights from Xenoliths, Orogenic Deep Sections, and Geophysical Studies
Anatomical Similarities and Differences Between Spatially Associated Porphyry Copper-Gold Deposits at the Reko Diq H14 and H15 Complex, Balochistan, Pakistan
Tectonics and Metallogeny of the Tethyan Orogenic Belt
The changing nature of sources associated with Columbia River flood basalts: Evidence from strontium isotope ratio variations in plagioclase phenocrysts
The Columbia River Flood Basalt Province
Phase transitions of minerals in the transition zone and upper part of the lower mantle
Advances in High-Pressure Mineralogy