Tectonic control on travertine and silica sinter deposition in oceanic transform-fault setting: the case of the Lýsuskarð volcano-geothermal area, Snæfellsnes Peninsula, Iceland ...
Deposition of terrestrial carbonate (i.e. travertine) and silica sinter in geothermal areas is always closely linked to the presence of relevant crustal structures which enhance the permeability in the upper crust favouring the upflow of fluids to the surface. Most travertine deposits are originated...
| Main Authors: | , , , |
|---|---|
| Format: | Dataset |
| Language: | unknown |
| Published: |
Taylor & Francis
2023
|
| Subjects: | |
| Online Access: | https://dx.doi.org/10.6084/m9.figshare.22134842 https://tandf.figshare.com/articles/dataset/Tectonic_control_on_travertine_and_silica_sinter_deposition_in_oceanic_transform-fault_setting_the_case_of_the_L_suskar_volcano-geothermal_area_Sn_fellsnes_Peninsula_Iceland/22134842 |
| Summary: | Deposition of terrestrial carbonate (i.e. travertine) and silica sinter in geothermal areas is always closely linked to the presence of relevant crustal structures which enhance the permeability in the upper crust favouring the upflow of fluids to the surface. Most travertine deposits are originated by geothermal fluids stored within carbonate reservoirs in continental crust, and their morphology and areal distribution provide useful information on geometry, kinematics, and age of faults which control the fluid flow. In this paper, we focus on the tectonic control on a travertine depositional system, associated with silica sinter, developing in oceanic crust, in the Lýsuskarð volcano-geothermal area on the Snæfellsnes Peninsula, West Iceland. The presence of HCO 3 and Ca in the geothermal fluids is related to chemical-physical processes linked to fluid–rock interaction that occurs in the geothermal reservoir made up of tholeiitic basalt, by fluids enriched in CO 2 of deep origin (i.e. magmatic). Travertine ... |
|---|