Zobrazeno 1 - 10
of 38
pro vyhledávání: '"Maarten Felix"'
Publikováno v:
Geosciences, Vol 14, Iss 9, p 232 (2024)
Carbonate muds are essential sedimentary components in geological carbon cycles. Model carbonate muds are prepared from crushed, sieved carbonate rock. The carbonate rock particles are primarily smaller than 62.5 µm. Steady-state shear viscosity was
Externí odkaz:
https://doaj.org/article/9feb257afb4d41a18eedc90612de46f5
Autor:
Maren Sandvold, Maarten Felix
The Nordkapp Basin is located in the southwest Barents Sea. It was formed by rifting in the late Palaeozoic. As the area containing the basin moved north from the equator the climate changed from warm and arid to temperate and humid. Initially a larg
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::969b9752857f6503b03f4ab762cbffda
https://doi.org/10.5194/egusphere-egu22-2502
https://doi.org/10.5194/egusphere-egu22-2502
Publikováno v:
Marine and Petroleum Geology. 102:704-724
The Permian Lucaogou Formation in the Jimusaer Sag of the southeastern Junggar Basin in China is an uncommon set of mixed sedimentary rocks. The mixed sediment content of the Lucaogou Formation is unusual due to the large amounts of tuffaceous materi
This project examines organic rich black shales from the Upper Jurassic on the Norwegian shelf. The aim is to investigate the relationship between the depositional environment as determined from facies descriptions and the magnetic properties of the
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::5475a106f59579361722e7eec6f49c2b
https://doi.org/10.5194/egusphere-egu2020-10406
https://doi.org/10.5194/egusphere-egu2020-10406
The Late Cretaceous Nise Formation is located on the Mid-Norwegian Continental Shelf. On the Halten Terrace, the formation is generally described as a mudstone interbedded with thin sandstones and carbonate stringers. The spatial distribution, connec
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::4c9232f34e2e8d5db7ff407a4cc91f15
https://doi.org/10.5194/egusphere-egu2020-20037
https://doi.org/10.5194/egusphere-egu2020-20037
Autor:
Emily Barnabas Kiswaka, Maarten Felix
Publikováno v:
Norwegian Journal of Geology
Seismic interpretation (2D and new 3D surveys) has been used to investigate sedimentary fills and timing of tectonic activity offshore Mid Norway. This study was focused on upper Permian and Lower Triassic sedimentary basin fills, but a longer strati
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::335f2bc1eb8603e21a72f3f7a633e08b
https://hdl.handle.net/11250/2994921
https://hdl.handle.net/11250/2994921
Autor:
Lolita Marheni, Stale Johansen, Dicky Harishidayat, Kamaldeen Olakunle Omosanya, P. Abrahamson, Maarten Felix
Publikováno v:
Marine Geology. 376:175-193
Mass-wasting on the NE Atlantic Margin is generally attributed to Cenozoic glaciations. Using high-quality 2D seismic datasets and two exploration wells, this study investigates the types and driving mechanisms of mass-wasting in the Sorvestsnaget Ba
Autor:
Emily Barnabas Kiswaka, Maarten Felix
Publikováno v:
Marine and Petroleum Geology. 119:104463
Seismic surveys of the Permo-Triassic successions in Norwegian Sea sub-basins have been studied to determine the distribution of organic-carbon-rich intervals in the deeper basinal areas. Upper Permian to Lower Triassic organic-carbon-rich deposits h
Publikováno v:
Climate of the Past, Vol 10, Iss 2, Pp 569-587 (2014)
There is generally a lack of knowledge on how marine organic carbon accumulation is linked to vertical export and primary productivity patterns in the Arctic Ocean. Despite the fact that annual primary production in the Arctic has increased as a cons
Autor:
Maarten Felix
Publikováno v:
Marine Geology. 347:1-11
A comparison is made of different methods for calculating total organic carbon (TOC) in deposits and marine primary productivity using sediment data. The calculation methods include both equations derived by pure regression analysis, and equations th