Journal
DATA IN BRIEF
Volume 31, Issue -, Pages -Publisher
ELSEVIER
DOI: 10.1016/j.dib.2020.105896
Keywords
Fluid flow; SE Pyrenees; U-Pb dating; Fluid geochemistry
Categories
Funding
- DGICYT Spanish Project Ministerio de Ciencia, Innovacion y Universidades/Agencia Estatal de Investigacion/Fondo Europeo de Desarrollo Regional [PGC2018-093903-B-C22]
- Union Europea, Alpimed [PIE-CSIC-201530E082]
- Union Europea, Subtetis project [PIE-CSIC-201830E039]
- Grup Consolidats de Recerca Geologia Sedimentaria [2017SGR-824]
- Geodinamica Interna [2017SGR-847]
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U-Pb dating using laser ablation-inductively coupled plasma mass spectrometry (LA-ICP-MS), delta C-13, delta O-18, clumped isotopes and Sr-87/Sr-86 analysis, and electron microprobe have been applied to fracture-filling calcites and host carbonates from the Lower Pedraforca thrust sheet, in the SE Pyrenees. These data are used to determine the type and origin of migrating fluids, the evolution of the palaeohydrological system and timing of fracturing during the emplacement of this thrust sheet, as described in the article From hydroplastic to brittle deformation: controls on fluid flow in fold and thrust belts. Insights from the Lower Pedraforca thrust sheet (SE Pyrenees) - Marine and Petroleum Geology (2020). The integration of these data is also used to compare the fluid flow evolution of the Southern Pyrenees with that of other orogens worldwide and to generate a fluid flow model in fold and thrust belts. At a more local scale, the U-Pb dataset provides new absolute ages recording the deformation in the Lower Pedraforca thrust sheet, which was previously dated by means of indirect methods such as biostratigraphy of marine sediments and magnetostratigraphy of continental deposits. (C) 2020 The Author(s). Published by Elsevier Inc.
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