New evidence concerning the thermal history of Devonian and Carboniferous rocks in the South Portuguese Zone
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- journal_title：Journal of the Geological Society
- Contributor：Paulo Fernandes ; Jennifer A. Musgrave ; Geoff Clayton ; Zélia Pereira ; José Tomás Oliveira ; Robbie Goodhue ; Bruno Rodrigues
- Publisher：Geological Society of London
- Date：2012-11-01
- Format：text/html
- Language：en
- Identifier：10.1144/jgs2011-156
- journal_abbrev：Journal of the Geological Society
- issn：0016-7649
- volume：169
- issue：6
- firstpage：647
- section：Research Article
摘要
<p id="p-1">The Late Palaeozoic rocks of southern Portugal have a complex thermal history. Vitrinite reflectance determinations from 90 samples confirm that the organic maturity of Late Palaeozoic rocks in SW Portugal is very high, mainly corresponding to meta-anthracite coal rank. The optic fabric of vitrinite in oriented coal samples from the Brejeira Formation suggests maturation under simple, non-tectonic, burial conditions with peak temperatures being attained prior to Variscan deformation. The lack of any increase in vitrinite reflectance with depth through c. 1 km of section in borehole AC-1 is not consistent with conductive heat transfer and is interpreted as the result of late synorogenic to post-orogenic advective heating. This heating episode generated temperatures sufficiently high to produce levels of maturity corresponding to meta-anthracite coal rank through much of the terrane now exposed, but not high enough to result in overprinting of the pre-deformation optic fabric of vitrinite in the thin coals. The slightly lower maturity of older, platform-facies rocks in the Aljezur–Bordeira area may reflect either deposition on a basement high followed by less burial than adjacent parts of the basin, or the area being the site of a sink for descending relatively cool fluids. p>