Major and trace element analyses of serpentinites from northern Apennine ophiolite, Italy
This data set presents Major and trace element analyses of fault rocks in serpentinitized peridotite and analyses of associated host serpentinites in Jurassic ophiolite in the northern Apennines, Italy. The fault rocks are altered to talc at depth, and are carbonated near the paleo seafloor. Carbonated serpentinite breccias are also present at the paleo seafloor.
How to cite this dataset:
Alt, J., 2020. Major and trace element analyses of serpentinites from northern Apennine ophiolite, Italy, Version 1.0. Interdisciplinary Earth Data Alliance (IEDA). https://doi.org/10.26022/IEDA/111685.
DOI Creation Date:
Alt, Jeff, Laura Crispini, Laura Gaggero, David Levine, Giorgia Lavagnino, Pat Shanks, and Cayce Gulbransen. Normal Faulting and Fluid Discharge in the Subsurface of a Jurassic Seafloor Ultramafic-Hosted Hydrothermal System, Northern Apennines, Italy, Geology 46 (6) , 523–526
Creative Commons Attribution-ShareAlike 4.0 International [CC-BY-SA-4.0]
Coverage Scope: Regional (Continents, Oceans)
Geographic Location: Apennine mountains, Italy,
User Contributed Keyword(s):
Serpentinite, fault rocks, hydrothermal, ophiolite
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