Major and trace element analyses of serpentinites from northern Apennine ophiolite, Italy

Creator(s):
Alt, Jeff
Abstract:
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. Accessed 2021-09-20.
DOI Creation Date:
2020-09-24
Related
Publication(s):
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
License:
Creative Commons Attribution-ShareAlike 4.0 International [CC BY-SA 4.0]
Funding source(s):
National Science Foundation: OCE-1536242
Keyword(s):
Coverage Scope: Regional (Continents, Oceans)
Geographic Location: Apennine mountains, Italy,
User Contributed Keyword(s):
Serpentinite, fault rocks, hydrothermal, ophiolite
Data Available On:
2020-09-24
Resource Type:
Dataset
Download File(s)
File Name
File Size
File Checksum
1685-1_ECL_Alt_Elemental_BulkSample.xls
227 KB

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