Harlov, Daniel E. (2000) Titaniferous magnetite–ilmenite thermometry and titaniferous magnetite–ilmenite–orthopyroxene–quartz oxygen barometry in granulite facies gneisses, Bamble Sector, SE Norway: implications for the role of high-grade CO2-rich fluids during granulite genesis. Contributions to Mineralogy and Petrology, 139 (2) 180-197 doi:10.1007/pl00007670

Reference Type | Journal (article/letter/editorial) | ||
---|---|---|---|
Title | Titaniferous magnetite–ilmenite thermometry and titaniferous magnetite–ilmenite–orthopyroxene–quartz oxygen barometry in granulite facies gneisses, Bamble Sector, SE Norway: implications for the role of high-grade CO2-rich fluids during granulite genesis | ||
Journal | Contributions to Mineralogy and Petrology | ||
Authors | Harlov, Daniel E. | Author | |
Year | 2000 (June 6) | Volume | 139 |
Issue | 2 | ||
Publisher | Springer Science and Business Media LLC | ||
DOI | doi:10.1007/pl00007670Search in ResearchGate | ||
Generate Citation Formats | |||
Mindat Ref. ID | 77890 | Long-form Identifier | mindat:1:5:77890:1 |
GUID | 0 | ||
Full Reference | Harlov, Daniel E. (2000) Titaniferous magnetite–ilmenite thermometry and titaniferous magnetite–ilmenite–orthopyroxene–quartz oxygen barometry in granulite facies gneisses, Bamble Sector, SE Norway: implications for the role of high-grade CO2-rich fluids during granulite genesis. Contributions to Mineralogy and Petrology, 139 (2) 180-197 doi:10.1007/pl00007670 | ||
Plain Text | Harlov, Daniel E. (2000) Titaniferous magnetite–ilmenite thermometry and titaniferous magnetite–ilmenite–orthopyroxene–quartz oxygen barometry in granulite facies gneisses, Bamble Sector, SE Norway: implications for the role of high-grade CO2-rich fluids during granulite genesis. Contributions to Mineralogy and Petrology, 139 (2) 180-197 doi:10.1007/pl00007670 | ||
In | (2000, June) Contributions to Mineralogy and Petrology Vol. 139 (2) Springer Science and Business Media LLC |
See Also
These are possibly similar items as determined by title/reference text matching only.