File:The Quarterly journal of the Geological Society of London (1881) (14584067458).jpg

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Identifier: quarterlyjourna371881geol (find matches)
Title: The Quarterly journal of the Geological Society of London
Year: 1845 (1840s)
Authors: Geological Society of London
Subjects: Geology
Publisher: London (etc.)
Contributing Library: Smithsonian Libraries
Digitizing Sponsor: Biodiversity Heritage Library

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t strata occurred before the deposition of the next series. The Khirthar series inclnd.es in its highest portion a massive, paleor dark grey, hard, compact jSTummulitic limestone whose extremethickness is 3000 feet. It thins out to the south-west, and disap-pears within a distance of twenty-five miles of its greatest develop-ment. Other ISFummulitic limestone-beds are found, which may belower in the series ; and they and the main group are representedelsewhere by shaly limestones and sandstones with calcareous bands.In some districts flint occurs in a limestone with Alveolince. Thelower members of the series are often wanting, and are well repre-sented by shales, marls, and sandstones and where these are present;unconformity with the underlying .Eanikot beds is not seen; butwhere they are absent the j^ummulitic limestone (as in the Lakirange) rests unconformably. The compact limestone is of course-* Memoirs Geol. Survey of India, vol. xvii, pt. 1, p. 131. 194 PROF. P. M. DUNCAN OX THE
Text Appearing After Image:
C0RALL1EE110US SERIES OF BIND. 195 highly fossiliferous; but it has not yielded very good specimens ofCorals. The indications of a fringing-reef-buildirig fauna, or a bankof coral, are distinct; but the species when compared with theirmodern analogues do not indicate a great reef-development.Amongst other fossils, Lamellibranchiata prevail, and the Echini arenumerous; but the jNumnnilitcs and Orbitolites, Alveolince, andPatellince are the most important organic remains. Amongst theNummiilites there are N. Bamondi, iV. biaritzensis, iV. Beaumonti,N. granulosus, and N. Leymeriei. The )STari series rests conformably on the Khirthars ; and there isoccasionally an apparent passage from the Khirthar limestone into ayellow or brown rock of the ISTari group. There is, however, abiological break; for the Juimmulites of the upper group arocharacteristic, and differ from those of the lower. The Khirtharforms are not found, and Nummidites garansensis appears with Orbi-toides pevpyracea, in the j^

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Author Geological Society of London
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Volume
InfoField
1881
Flickr tags
InfoField
  • bookid:quarterlyjourna371881geol
  • bookyear:1845
  • bookdecade:1840
  • bookcentury:1800
  • bookauthor:Geological_Society_of_London
  • booksubject:Geology
  • bookpublisher:London__etc__
  • bookcontributor:Smithsonian_Libraries
  • booksponsor:Biodiversity_Heritage_Library
  • bookleafnumber:241
  • bookcollection:biodiversity
  • BHL Collection
  • BHL Consortium
Flickr posted date
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28 July 2014
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