Paris Basin (geology)

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The Paris Basin is one of the major geological regions of France having developed since the Triassic on a basement formed by the Variscan orogeny. The sedimentary basin is a large sag in the craton, bordered by the Armorican Massif to the west, the Ardennes-Brabant axis to the north, the Massif des Vosges to the east, and the Massif Central to the south.[1]:252

Extent[edit]

The region usually regarded as the Paris Basin is rather smaller than the area formed by the geological structure. The former occupies the centre of the northern half of the country, excluding Eastern France. The latter extends from the hills just south of Calais to Poitiers and from Caen to the brink of the middle Rhine Valley, east of Saarbrücken.

Geography[edit]

The countryside is one of plains and plateaux of limited altitude. In the south-east and east the plain of Champagne and the Seuil de Bourgogne (Threshold of Burgundy) differential erosion of the strata has left low scarps with the dip slopes towards the centre. The varying nature of the clays, limestones and chalk gives rise to the characteristics of the regions such as Champagne Humide (Damp Champagne), Champagne Pouilleuse (poor Champagne),[2] the Pays de Caux and the Pays de Bray. Map missing

Structure[edit]

The Paris Basin is a geological basin of sedimentary rocks. It overlies geological strata disturbed by the Variscan orogeny and forms a broad shallow bowl in which successive marine deposits from throughout periods from the Triassic to the Pliocene were laid down, their extent generally diminishing with time. Based on his analysis of fossils he recognized in the Paris Basin strata during the 1820s and 30s, the pioneering geologist Charles Lyell divided the Tertiary into three ages he named the Pliocene, the Miocene and the Eocene. .

To the west, the strata folded by the Variscan rise from below the more recent marine deposits in the hills of Brittany and, to the east, the Ardennes, Hunsrück and Vosges. To the south, it borders on the Massif Central and the Morvan. To the north, its strata link into those of the bed of the English Channel and south-eastern England. Other boundaries lie on ridges in more recent deposits and scarps such as the Côte d'Or (on an Alpine fault line) and the Hills of Artois which overlie the margin of London-Brabant Massif.

Oil Fields[edit]

Two large oil fields are located in the basin, one is the Chaunoy Field, the other is the Villeperdue Field, discovered in 1982.[1]:254 The Villeperdue produces from a Middle Jurassic oolitic limestone 1850 m deep.[1]:251

See also[edit]

References[edit]

  1. ^ a b c Duval, B.C., 1992, Villeperdue Field, In Giant Oil and Gas Fields of the Decade, 1978-1988, AAPG Memoir 54, Halbouty, M.T., editor, Tulsa: American Association of Petroleum Geologists, ISBN0891813330
  2. ^ Pouilleuse means 'lousy' that is, 'infested with lice' but its meaning has broadened in use to include 'down and out'. This is a region of thin, chalk soils and little surface water. The epithet indicates the extreme poverty of the region when the name was acquired.
  • Anon. Carte Géologique de la France à l'Échelle du Millionième ISBN 2-7159-2158-6
  • Dercourt, J. (2002). Géologie et Géodynamique de la France (3rd ed.). ISBN 2-10-006459-2.