Oxfordian neptunian dykes with brachiopods from the southern part of the Kraków-Częstochowa Upland (southern Poland) and their links to hydrothermal vents-Reference-Cited by-同舟云学术

Oxfordian neptunian dykes with brachiopods from the southern part of the Kraków-Częstochowa Upland (southern Poland) and their links to hydrothermal vents

Published:2016-03-09 Issue:2 Volume:62 Page:
ISSN:0172-9179
Container-title:Facies
language:en
Short-container-title:Facies

Author:

Matyszkiewicz Jacek,Krajewski Marcin,Kochman Alicja,Kozłowski Andrzej,Duliński Marek

Funder

Narodowe Centrum Nauki

Publisher

Springer Science and Business Media LLC

Subject

Paleontology,Stratigraphy,Geology

Link

http://link.springer.com/content/pdf/10.1007/s10347-016-0464-x.pdf

Reference150 articles.

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3. Allenbach RP (2002) The ups and downs of ‘Tectonic Quiescence’—recognizing differential subsidence in the epicontinental sea in the Oxfordian in the Swiss Jura Mountains. Sediment Geol 150:323–342

4. Asgaard U (1968) Brachipod palaeoecology in Middle Danian limestones at Fakse, Denmark. Lethaia 1:103–121

5. Ayoub-Hannaa W, Radulović BV, Radulović VJ, Fürsich FT, Vasić N (2014) Brachiopods and echinoids from the lower Cenomanian of Koraćica (Kosmaj Mountain, central Serbia). Cretac Res 51:121–147

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