Atmospheric contamination of the primary Ne and Ar signal in mid-ocean ridge basalts and its implications for ocean crust formation

Author:

Stroncik N.A.,Niedermann S.

Funder

Deutsche Forschungsgemeinschaft

Publisher

Elsevier BV

Subject

Geochemistry and Petrology

Reference75 articles.

1. Depths of partial crystallization of H2O-bearing MORB: phase equilibria simulations of basalts at the MAR near Ascension Island (7 11S);Almeev;J. Petrol.,2007

2. Amante, C. and Eakins B. W. (2009) ETOPO1 1 Arc-Minute Global Relief Model: Procedures, Data Sources and Analysis. NOAA Technical Memorandum NESDIS NGDC-24. National Geophysical Data Center, NOAA. doi: http://dx.doi.org/10.7289/V5C8276M.

3. Bach W. and Erzinger J. (1995) Volatile components in basalts and basaltic glasses from the EPR at 9°30′N. In Proceedings of the Ocean Drilling Program, Scientific Results (eds. R. Batiza, M. A. Storms, and J. F. Allan). 142, pp. 23–29.

4. The origin of air-like noble gases in MORB and OIB;Ballentine;Earth Planet. Sci. Lett.,2000

5. Production, release and transport of noble gases in the continental crust;Ballentine;Rev. Mineral. Geochem.,2002

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