Turbiditic and Pelagic Upper Cretaceous Oceanic Red Beds in the Romanian Carpathians
Upper Cretaceous Red Beds are widely distributed in the former Tethyan Realm, in the European, Asian and Central North Atlantic regions. This type of sedimentation followed in many regions the Lower Cretaceous Black Shales, indicating the replacement of an anoxic regime with an oxic one. For a bette...
Main Authors: | , , , , |
---|---|
Format: | Article in Journal/Newspaper |
Language: | unknown |
Published: |
2004
|
Subjects: | |
Online Access: | https://zenodo.org/record/57514 https://doi.org/10.5281/zenodo.57514 |
id |
ftzenodo:oai:zenodo.org:57514 |
---|---|
record_format |
openpolar |
spelling |
ftzenodo:oai:zenodo.org:57514 2023-05-15T17:33:21+02:00 Turbiditic and Pelagic Upper Cretaceous Oceanic Red Beds in the Romanian Carpathians MELINTE, Mihaela Carmen BRUSTUR, Titus JIPA, Dan SZOBOTKA, Stefan ANGHELUŢĂ, Cristina 2004-12-31 https://zenodo.org/record/57514 https://doi.org/10.5281/zenodo.57514 unknown https://zenodo.org/record/57514 https://doi.org/10.5281/zenodo.57514 oai:zenodo.org:57514 info:eu-repo/semantics/openAccess Geo-Eco-Marina No 9-10/2004 (2004) Upper Cretaceous red beds Romanian Carpathians info:eu-repo/semantics/article publication-article 2004 ftzenodo https://doi.org/10.5281/zenodo.57514 2023-03-11T00:32:51Z Upper Cretaceous Red Beds are widely distributed in the former Tethyan Realm, in the European, Asian and Central North Atlantic regions. This type of sedimentation followed in many regions the Lower Cretaceous Black Shales, indicating the replacement of an anoxic regime with an oxic one. For a better understanding of causes which produced such changes in deposition, the Upper Cretaceous Red Beds were intensively studied since 2002, by the participants in the IGCP-UNESCO Project 463-Upper Cretaceous Oceanic Red Beds: Response to Ocean/Climate Change (CORB). The Third Workshop of this Project was held in Romania in 2004, the one-day conference being followed by a three-day field trip in the Romanian Carpathians. Most of the investigated sections in the field are situated in the Bend Area of the Romanian Carpathians. Upper Cretaceous Red Beds from the above-mentioned region display various facies (pelagic/hemipelagic, turbiditic), covering the interval Cenomanian-Maastrichtian (including the K/T boundary interval). The causes which produce this type of sedimentation are various. Changes in geoechemical regime, in palaeoproductivity of surface waters as well as in palaeogeography were assumed to interact. Article in Journal/Newspaper North Atlantic Zenodo |
institution |
Open Polar |
collection |
Zenodo |
op_collection_id |
ftzenodo |
language |
unknown |
topic |
Upper Cretaceous red beds Romanian Carpathians |
spellingShingle |
Upper Cretaceous red beds Romanian Carpathians MELINTE, Mihaela Carmen BRUSTUR, Titus JIPA, Dan SZOBOTKA, Stefan ANGHELUŢĂ, Cristina Turbiditic and Pelagic Upper Cretaceous Oceanic Red Beds in the Romanian Carpathians |
topic_facet |
Upper Cretaceous red beds Romanian Carpathians |
description |
Upper Cretaceous Red Beds are widely distributed in the former Tethyan Realm, in the European, Asian and Central North Atlantic regions. This type of sedimentation followed in many regions the Lower Cretaceous Black Shales, indicating the replacement of an anoxic regime with an oxic one. For a better understanding of causes which produced such changes in deposition, the Upper Cretaceous Red Beds were intensively studied since 2002, by the participants in the IGCP-UNESCO Project 463-Upper Cretaceous Oceanic Red Beds: Response to Ocean/Climate Change (CORB). The Third Workshop of this Project was held in Romania in 2004, the one-day conference being followed by a three-day field trip in the Romanian Carpathians. Most of the investigated sections in the field are situated in the Bend Area of the Romanian Carpathians. Upper Cretaceous Red Beds from the above-mentioned region display various facies (pelagic/hemipelagic, turbiditic), covering the interval Cenomanian-Maastrichtian (including the K/T boundary interval). The causes which produce this type of sedimentation are various. Changes in geoechemical regime, in palaeoproductivity of surface waters as well as in palaeogeography were assumed to interact. |
format |
Article in Journal/Newspaper |
author |
MELINTE, Mihaela Carmen BRUSTUR, Titus JIPA, Dan SZOBOTKA, Stefan ANGHELUŢĂ, Cristina |
author_facet |
MELINTE, Mihaela Carmen BRUSTUR, Titus JIPA, Dan SZOBOTKA, Stefan ANGHELUŢĂ, Cristina |
author_sort |
MELINTE, Mihaela Carmen |
title |
Turbiditic and Pelagic Upper Cretaceous Oceanic Red Beds in the Romanian Carpathians |
title_short |
Turbiditic and Pelagic Upper Cretaceous Oceanic Red Beds in the Romanian Carpathians |
title_full |
Turbiditic and Pelagic Upper Cretaceous Oceanic Red Beds in the Romanian Carpathians |
title_fullStr |
Turbiditic and Pelagic Upper Cretaceous Oceanic Red Beds in the Romanian Carpathians |
title_full_unstemmed |
Turbiditic and Pelagic Upper Cretaceous Oceanic Red Beds in the Romanian Carpathians |
title_sort |
turbiditic and pelagic upper cretaceous oceanic red beds in the romanian carpathians |
publishDate |
2004 |
url |
https://zenodo.org/record/57514 https://doi.org/10.5281/zenodo.57514 |
genre |
North Atlantic |
genre_facet |
North Atlantic |
op_source |
Geo-Eco-Marina No 9-10/2004 (2004) |
op_relation |
https://zenodo.org/record/57514 https://doi.org/10.5281/zenodo.57514 oai:zenodo.org:57514 |
op_rights |
info:eu-repo/semantics/openAccess |
op_doi |
https://doi.org/10.5281/zenodo.57514 |
_version_ |
1766131837252403200 |