Open Circulation Facies in the Cenomanian of the Northeastern Margin of the Friuli Platform: the Iudrio Valley Case (NE Italy)

Item

Title (Dublin Core)

Description (Dublin Core)

<div>The Early Middle Cenomanian margin sequence of Val ludrio, connected with the northeastem margin of the Friuli Platform shows intercalated layers with pelagic organisms: Calcisphaerulidae and planktonic forams, among which is Favwsella. These are interpreted as transgressive episodes recorded in a calbonate ramp sequence related to a tectonically subsiding margin. ln the Dinaric and Friuli Platforms two distinct Calcisphaerulidae and planktonic forams facies are distinguished for the Cenomanian. The first one, of early-middle Cenomanian age, which is also present in the ludrio sequence, developed in platform margin zones subjected to drawning. The second one, of late Cenomanian age, developed in more internal areas of the Dinaric and Friuli Platforms, and can be related to the transgression</div><div>associated with the OAE 2 event.</div>

Creator (Dublin Core)

Dario Sartorio

Giorgio Tunis

Sandro Venturini

Subject (Dublin Core)

Early-Middle Cenomanian

Margin Sequence

Friuli Platform

Calcisphaerulidae

Favusella

transgressive events

Geology

QE1-996.5

Publisher (Dublin Core)

Croatian Geological Survey

Date (Dublin Core)

2010-12-01T00:00:00Z

Type (Dublin Core)

article

Identifier (Dublin Core)

1330-030X

1333-4875

10.4154/GC.1992.07

https://doaj.org/article/5d2190729cb54e628648a74c8c21c5bc

Source (Dublin Core)

Geologia Croatica, Vol 45, Iss 0, Pp 87-93 (2010)

Language (Dublin Core)

Relation (Dublin Core)

http://www.geologia-croatica.hr/ojs/index.php/GC/article/view/466

https://doaj.org/toc/1330-030X

https://doaj.org/toc/1333-4875

Provenance (Dublin Core)

Journal Licence: CC BY