Estimación del régimen térmico y producción de calor de los niveles litosféricos del Sistema Central Español

Simple item page
dc.contributor.authorVillaseca, Carlos
dc.contributor.authorOrejana, David
dc.contributor.authorPérez Soba, C.
dc.contributor.authorReyes Abril, J.
dc.date.accessioned2014-08-07T10:21:22Z
dc.date.available2014-08-07T10:21:22Z
dc.date.issued2005
dc.description.abstractHeat production of outcropping metamorphic and granitic rocks from the Spanish Central System (SCS) is similar to other surface heat production estimates in Paleozoic provinces (average A value 2.64 mWm-3). However, heat flow range in the SCS is higher than for Paleozoic terranes (70-90 mWm-2 instead of 45-70 mWm-2). Contribution of mantle to the heat budget is estimated to be 27 mWm-2. Thus, a slightly higher mantle heat flow combined with a lower crust with a markedly high heat production (average A value 1.04 mWm-3) may explain the high estimated surface heat flowen_US
dc.identifier.urihttp://hdl.handle.net/10272/8713
dc.language.isospaen_US
dc.publisherSociedad Geológica de Españaen_US
dc.rightsAtribución-NoComercial-SinDerivadas 3.0 España
dc.rights.accessRightsopen accessen_US
dc.rights.urihttp://creativecommons.org/licenses/by-nc-nd/3.0/es/
dc.subject.otherHeat flowen_US
dc.subject.otherHeat productionen_US
dc.subject.otherContinental crusten_US
dc.subject.otherSpanish Central Systemen_US
dc.titleEstimación del régimen térmico y producción de calor de los niveles litosféricos del Sistema Central Españolen_US
dc.titleThermal regime and heat production estimates for lithospheric levels of the Spanish Central Systemeng
dc.typejournal articleen_US
dspace.entity.typePublication

Files

Original bundle

Now showing 1 - 1 of 1
Thumbnail Image
Name:
Estimacion.pdf
Size:
214.91 KB
Format:
Adobe Portable Document Format
Download

Collections

Geogaceta -- Nº 38, (2005)