Mineralogical and geochemical evolution of micas from miarolitic pegmatites of the anorogenic pikes peak batholith, Colorado

Author:

Foord E. E.,Černý P.,Jackson L. L.,Sherman D. M.,Eby R. K.

Publisher

Springer Science and Business Media LLC

Subject

Geochemistry and Petrology,Geophysics

Reference54 articles.

1. Bailey SW (1984) Appendix 2-X-ray identification of mica polytypes: In:Bailey SW (ed) Reviews in mineralogy, vol 13. Micas. Mineral Soc of America, 10 pp

2. Barker F, Wones DR, Sharp WN, Desborough GA (1975) The Pikes Peak Batholith, Colorado Front Range, and a model for the origin of the gabbro-anorthosite-syenite-potassic granite suite. Precam Res 2: 97–160

3. Blasi A, Brajkovic A, De Pol Blasi C, Foord EE, Martin RF, Zanazzi PF (1984) Structure refinement and genetic aspects of a microcline overgrowth on amazonite from Pikes Peak batholith, Colorado, U.S.A. Bull de Mineral 107: 411–422

4. Černý P (1991a) Rare-element granitic pegmatites, part I. Anatomy and internal evolution of pegmatite deposits. Geosci Canada 18: 49–67

5. Černý P (1991b) Rare-element granitic pegmatites, part II. Regional to global environments and petrogenesis. Geosci Canada 18: 68–81

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