Erwan MARTIN

Department of Geological Sciences
1272 University of Oregon
Eugene, OR-97403 (USA)

e-mail: ermartin@uoregon.edu

Born: October 31, 1979
Nationality: French

- EDUCATION -

Stable Isotope lab at the Univerity of Oregon


- EXPERIENCES -


- SKILLS -


- EXTRA-CURRICULAR ACTIVITIES -

 

- PUBLICATIONS -

Martin E. & Sigmarsson O. (2005). Trondhjemitic and granitic melts formed by fractional crystallization of an olivine tholeiite from Reykjanes Peninsula, Iceland. Geological magazine, 142, 651-658. [pdf]

Martin E. (2006). Etude géochimique des magmas acides d'Islande : mode de genèse, implications sur l'évolution géodynamique islandaise et sur la formation de la proto-croûte continentale. Université Blaise Pascal, Clermont Ferrand, 272 pp.

Martin E. & Sigmarsson O. (2007). Crustal thermal state and origin of silicic magma in Iceland: the case of Torfajökull, Ljósufjöll and Snæfellsjökull volcanoes. Contribution to Mineralogy and Petrology, 153, 593-605. [pdf]

Martin, E. & Sigmarsson, O. (2007). Low-pressure differentiation of tholeiitic lavas as recorded in segregation veins from Reykjanes (Iceland), Lanzarote (Canary Islands) and Masaya (Nicaragua). Contribution to Mineralogy and Petrology. 154, 559-573. [pdf]

Martin E., Martin H. & Sigmarsson (2007). Could Iceland be a modern analogue of Earth's early continental crust? Accepted to Terra Nova.

Martin E., Bindeman I. & Grove T. (2008). Subduction in high fluid fluxing environment and the origin of high-d18O lavas in Mt. Shasta, Cascade arc, California. Submitted to Geochimica and Cosmochimica Acta.

Martin E. & Sigmarsson O. (2008). Overview of silicic magma composition produced during the last 15 Ma in Iceland.To submit to Journal of Petrology.

- CONFERENCES -

Martin E. & Sigmarsson O. (2005). Implication for the origin of tholeiitic silicic magmas from atmospheric pressure fractional crystallization of basaltic lava flows on Reykjanes peninsula (Iceland), Lanzarote (Canary Islands) and Masaya (Nicaragua). Geophysical Research Abstracts, 7, 00846, EGU General Assembly 2005, Vienna (Austria). Talk: [Abstract.pdf]

Martin E. & Sigmarsson O. (2006). Segregation veins in tholeiitic lavas: implications for the formation of silicic magmas in Iceland and for the genesis of primitive continental crust on the earth. Raunvísindaþing í Reykjavík (Iceland). [Poster.pdf]

Martin E. & Sigmarsson O. (2006). Crustal thermal state and origin of silicic magma in Iceland: the case of Torfajökull, Ljósufjöll and Snæfellsjökull volcanoes. RST, Dijon (France). [Poster.pdf]

Martin E. & Sigmarsson O. (2006). Trondhjemitic melts produced by in-situ differentiation of a tholeiitic lava flow, Reykjanes Peninsula, Iceland. AGU fall meeting, San Francisco (USA). [Poster.pdf]

Martin E., Bindeman I. & Grove T. (2007). Light stable isotopes constrain on slab fluids composition and behavior in a warm subduction zone: case of the Mount Shasta stratovolcano, California. MAG2007, Taipei (Taiwan). [Poster.pdf]

Martin E., Bindeman I. & Grove T. (2007). Subduction in high fluid fluxing environment and the origin of high-δ18O and high-δ7Li lavas in Mt. Shasta, Cascade arc, California. AGU fall meeting, San Francisco (USA). Talk: [Abstract.pdf]

Martin E. & Bindeman I. (2008). Detailed “supervolcanic” ash record in dry Lake Tecopa, California: δ34S, δ18O and Δ17O of soluble volcanic sulfate. Goldschmidt, Vancouver (CAN). [Abstract.pdf]

Martin E. & Bindeman I. (2008). Rare isotope insights into supereruption: sulfur and triple isotope geochemistry of sulfate aerosols absorbed on volcanic ash particules. IAVCEI, Reykjavik (Iceland).[Abstract.pdf]

Martin E. & Sigmarsson O. (2008). Overview of silicic magma composition produced during the last 15 Ma in Iceland. IAVCEI, Reykjavik (Iceland).[Abstract.pdf]