Origin of titanian pargasite in gabbroic rocks from the Northern Apennine ophiolites (Italy): insights into the late-magmatic evolution of a MOR-type intrusive sequence
- 13 March 2000
- journal article
- Published by Elsevier BV in Earth and Planetary Science Letters
- Vol. 176 (3-4), 281-293
- https://doi.org/10.1016/s0012-821x(00)00014-5
Abstract
No abstract availableKeywords
This publication has 34 references indexed in Scilit:
- Evolution of gabbroic rocks of the Northern Apennine ophiolites (Italy): Comparison with the lower oceanic crust from modern slow-spreading ridgesPublished by Geological Society of America ,2000
- Fluid evolution in slow-spreading environmentsPublished by International Ocean Discovery Program (IODP) ,1997
- Rare Earth Element Constraints on the Origin of Amphibole in Gabbroic Rocks from Site 894, Hess DeepPublished by International Ocean Discovery Program (IODP) ,1996
- Melt-Fluid Evolution in Gabbroic Rocks from Hess DeepPublished by International Ocean Discovery Program (IODP) ,1996
- Petrology and Geochemistry of Gabbroic and Related Rocks from Site 894, Hess DeepPublished by International Ocean Discovery Program (IODP) ,1996
- Rare earth element redistribution during high-pressure–low-temperature metamorphism in ophiolitic Fe-gabbros (Liguria, northwestern Italy): Implications for light REE mobility in subduction zonesGeology, 1996
- Determination of hydrogen in silicates by secondary ion mass spectrometryThe Analyst, 1995
- Alpine Jurassic ophiolites resemble the modern central Atlantic basementGeology, 1990
- Chemical differentiation of the Earth: the relationship between mantle, continental crust, and oceanic crustEarth and Planetary Science Letters, 1988
- The O, Sr, Nd and Pb isotope geochemistry of MORBChemical Geology, 1987