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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
254:(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.
228:to the brink of the middle Rhine Valley, east of
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240:The landscape is one of very broad valleys (
171:) is one of the major geological regions of
357:into three ages he named the Pliocene, the
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27:Major geological region of France
334:folded by the Variscan orogeny.
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435:Two notable oil fields are the
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295:And three flowing west, the:
568:Sedimentary basins of Europe
423:which overlie the margin of
179:over remnant uplands of the
138:Knowledge (XXG):Translation
97:will aid in categorization.
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183:(Hercynian orogeny). The
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262:(poor Champagne), the
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529:Dercourt, J. (2002).
461:(with link directory)
425:London-Brabant Massif
319:The Paris Basin is a
203:to the east, and the
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458:List of fossil sites
260:Champagne Pouilleuse
558:Geography of France
453:Geologic time scale
439:, the other is the
396:and south-eastern
258:(Damp Champagne),
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441:Villeperdue Field
328:sedimentary rocks
201:Massif des Vosges
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417:Collines d'
300:Seine basin
230:Saarbrücken
161:Paris Basin
155:Paris Basin
56:(July 2016)
552:Categories
499:Pouilleuse
488:0891813330
467:References
431:Oil fields
409:fault line
321:geological
306:basin and
302:, central
288:and upper
502:acquired.
402:Côte d'Or
315:Structure
247:Champagne
236:Geography
224:and from
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83:Consider
51:in French
447:See also
388:and the
378:Hunsrück
374:Ardennes
370:Brittany
361:and the
355:Tertiary
343:Pliocene
339:Triassic
268:and the
250:and the
222:Poitiers
177:Triassic
107:provide
510:Sources
398:England
359:Miocene
347:fossils
341:to the
286:Moselle
129:to the
111:in the
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515:Anon.
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421:Artois
413:French
406:Alpine
390:Morvan
382:Vosges
363:Eocene
332:strata
284:upper
218:Calais
211:Extent
193:craton
173:France
165:French
324:basin
308:Somme
304:Loire
290:Meuse
74:DeepL
535:ISBN
520:ISBN
484:ISBN
380:and
226:Caen
159:The
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