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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
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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
243:(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
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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,
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Do not translate text that appears unreliable or low-quality. If possible, verify the text with references provided in the foreign-language article.
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Due to the millions of years of later deposition, erosion and other changes since, five drainage basins today drain almost all of the Basin.
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Content in this edit is translated from the existing French
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To the west, the strata folded by the
Variscan rise below the more recent marine deposits in the hills of
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It forms a broad shallow bowl in which marine deposits from throughout periods from the
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recognized in the basin's strata during the 1820s and 1830s, the pioneering geologist
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were laid down. Their extent generally decreases with time. Based on analysis of
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These are two flowing north, the basins/specified parts of basins as follows:
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to the west, the
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Carte Géologique de la France à l'Échelle du
Millionième
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a machine-translated version of the French article.
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229:The landscape is one of very broad valleys (
160:) is one of the major geological regions of
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16:Major geological region of France
323:folded by the Variscan orogeny.
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424:Two notable oil fields are the
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284:And three flowing west, the:
557:Sedimentary basins of Europe
412:which overlie the margin of
168:over remnant uplands of the
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450:(with link directory)
414:London-Brabant Massif
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447:List of fossil sites
249:Champagne Pouilleuse
547:Geography of France
442:Geologic time scale
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385:and south-eastern
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241:Seuil de Bourgogne
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430:Villeperdue Field
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406:Collines d'
289:Seine basin
219:Saarbrücken
150:Paris Basin
144:Paris Basin
45:(July 2016)
541:Categories
488:Pouilleuse
477:0891813330
456:References
420:Oil fields
398:fault line
310:geological
295:basin and
291:, central
277:and upper
491:acquired.
391:Côte d'Or
304:Structure
236:Champagne
225:Geography
213:and from
120:talk page
72:Consider
40:in French
436:See also
377:and the
367:Hunsrück
363:Ardennes
359:Brittany
350:and the
344:Tertiary
332:Pliocene
328:Triassic
257:and the
239:and the
211:Poitiers
166:Triassic
96:provide
499:Sources
387:England
348:Miocene
336:fossils
330:to the
275:Moselle
118:to the
100:in the
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504:Anon.
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410:Artois
402:French
395:Alpine
379:Morvan
371:Vosges
352:Eocene
321:strata
273:upper
207:Calais
200:Extent
182:craton
162:France
154:French
313:basin
297:Somme
293:Loire
279:Meuse
63:DeepL
524:ISBN
509:ISBN
473:ISBN
369:and
215:Caen
148:The
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