Asynchronous infiltration-driven growth of forsterite and periclase during metamorphism in marbles of the inner Alta aureole, Utah: δ18O and textural records of oxygen isotope disequilibrium, rapid forsterite growth and reaction history

Author:

Beno Carl J.ORCID,Bowman John R.,Kitajima KoukiORCID,Valley John W.ORCID,Loury Patrick C.,Tapanila Lorraine M.

Funder

Division of Earth Sciences

Publisher

Springer Science and Business Media LLC

Subject

Geochemistry and Petrology,Geophysics

Reference76 articles.

1. Bakshi MS (2016) How surfactants control crystal growth of nanomaterials. Cryst Growth Des 16:1104–1133

2. Baker AA, Calkins FC, Crittenden MD, Bromfield CS (1966) Geologic map of the Brighton quadrangle. U.S. Geological Survey Map GQ-535, Utah

3. Bennema P, van der Eerden JP (1987) Crystal graphs, connected nets, roughening transition and the morphology of crystals. In: Sunagawa I (ed) Morphology of crystals: part A. Terra Scientific, Tokyo, Japan, pp 1–75

4. Beno CJ, Bowman JR, Loury PC, Tapanila LM, Fernandez DP (2020) Evidence for dendritic crystallization of forsterite olivine during contact metamorphism of siliceous dolostones, alta stock aureole. Utah Contrib Miner Petrol 175:93

5. Berman RG (1988) Internally-consistent thermodynamic data for minerals in the system Na2O-K2O-CaO-MgO-FeO-Fe2O3-Al2O3-SiO2-TiO2-H2O-CO2. J Petrol 29:445–522

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