Evidence and effects of fluid circulation on organic matter in intramontane coalfields (Massif Central, France)

Citation
Y. Copard et al., Evidence and effects of fluid circulation on organic matter in intramontane coalfields (Massif Central, France), INT J COAL, 44(1), 2000, pp. 49-68
Citations number
53
Categorie Soggetti
Earth Sciences
Journal title
INTERNATIONAL JOURNAL OF COAL GEOLOGY
ISSN journal
01665162 → ACNP
Volume
44
Issue
1
Year of publication
2000
Pages
49 - 68
Database
ISI
SICI code
0166-5162(200007)44:1<49:EAEOFC>2.0.ZU;2-6
Abstract
Recent evidence for a Late Carboniferous hydrothermal event responsible for Au-As mineralization within the Variscan belt of the French Massif Central adds a supplementary episode to the already rather complex thermal history of this area. To better understand this history, 45 coal samples from vari ous sites in the Massif Central were studied petrographically (reflectance analysis) and geochemically (Rock-Eval pyrolysis). The results of this stud y suggest that the studied coal was buried to 1500 m and that the coalifica tion took place within 25 Ma, probably ending at the boundary between the E arly and Late Permian (marked by the Saalic orogeny). Two thermal end-membe rs basins were identified: (i) the Carboniferous of Bosmoreau-les-Mines (Li mousin) and West Graissessac (Montagne Noire) showing geothermal paleoflow values between 150 and 180 mW m(-2), and (ii) the Stephanian of Argentat an d Detroit de Rodez (SW Massif Central) with values estimated at between 100 and 120 mW m(-2). By plotting the T-max and R-o values on a diagram, the s amples were grouped into two populations, the first showing a positive corr elation between R-o and T-max and the second with higher T-max values than expected after R-o values. Selected samples of the second group are also ch aracterized by a high Oxygen Index (OI) that increases with T-max. These di vergence between R-o and T-max associated with a high OI may be the result of the circulation of slightly oxidizing hot fluids subsequent to coalifica tion. The other kind of R-o-T-max divergence seems to be linked to local, p articularly high thermal activity, especially in Graissessac and Bosmoreau basins. It is interpreted as being due to a difference in response of these two maturity indicators, respectively to the intensity and duration of the thermal events (e.g., shore-lived hydrothermal circulation and thermal dom es of regional extent). (C) 2000 Elsevier Science B.V. All rights reserved.