Zobrazeno 1 - 9
of 9
pro vyhledávání: '"Martin Nauton"'
Publikováno v:
The Depositional Record, Vol 7, Iss 1, Pp 52-63 (2021)
Abstract Sandstone composition is influenced by multiple factors, including acidic weathering, occurring during storage in the hinterland, prior to deposition. This study aims to better understand and constrain how the nature and duration of such pre
Externí odkaz:
https://doaj.org/article/8fab8ca6d65042c8a5f7e3acacb1ffff
The west coast of Ireland is currently one of the wettest environments in Europe, with year-round precipitation, high humidity, and minimal thermal seasonality maintained by a strongly North Atlantic climate. While such conditions are not conducive t
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::1e0afb26318ba463518afb68825881cd
https://doi.org/10.5194/egusphere-egu23-17138
https://doi.org/10.5194/egusphere-egu23-17138
Publikováno v:
The Depositional Record, Vol 7, Iss 1, Pp 52-63 (2021)
The Depositional Record
The Depositional Record
Sandstone composition is influenced by multiple factors, including acidic weathering, occurring during storage in the hinterland, prior to deposition. This study aims to better understand and constrain how the nature and duration of such pre‐deposi
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::f8c961f32f14639e7bfbe2d0c32c2a33
https://doi.org/10.1002/dep2.128
https://doi.org/10.1002/dep2.128
Autor:
Martin Nauton-Fourteu, Shane Tyrrell, David Chew, Andrew C. Morton, Gary O'Sullivan, Chris Mark
Publikováno v:
Basin Research. 33:342-363
[Abstract Quartz‐rich sandstones can be produced through multiple sedimentary processes, potentially acting in combination, such as extensive sedimentary recycling or intense chemical weathering. Determining the provenance of such sedimentary rocks
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::a834d6febac3c24b0939b05a77283bc5
https://doi.org/10.1111/bre.12469
https://doi.org/10.1111/bre.12469
Publikováno v:
Geological Journal. 55:5432-5450
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::4372e9f1c6e1e184c9e466060cc72f61
https://doi.org/10.1002/gj.3697
https://doi.org/10.1002/gj.3697
Autor:
Martin Nauton-Fourteu, David Chew, Katharina Pfaff, Shane Tyrrell, Zane R. Jobe, Foteini Drakou
Publikováno v:
Journal of the Geological Society. 178
In a source-to-sink sedimentary system, multiple processes have the potential to modify the sediment composition during sediment generation at the source, through transport, deposition and burial. To investigate these issues, a multi-proxy provenance
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::bd9e21c2d280dd7dabfa91d588e65d43
https://doi.org/10.1144/jgs2020-216
https://doi.org/10.1144/jgs2020-216
Publikováno v:
Atlantic Geology. :409-470
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::4777d7f7ace92606d349fa62c5df0d9c
https://doi.org/10.4138/atlgeol.2018.014
https://doi.org/10.4138/atlgeol.2018.014
Autor:
Shane Tyrrell, Andrew C. Morton, Aoife Blowick, David Chew, Martin Nauton-Fourteu, Bébhinn Anders, Jess Franklin
Publikováno v:
Geological Society of America Abstracts with Programs.
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::8c27d63e176bad2392b3fcb5eb63096f
https://doi.org/10.1130/abs/2019am-335946
https://doi.org/10.1130/abs/2019am-335946
Controls on the provenance of late Eocene to Quaternary Mozambique Channel shales (DSDP 25 Site 242)
Autor:
Martin Nauton-Fourteu, Martin Roddaz, Roberto Ventura Santos, Elton Luiz Dantas, Gérôme Calvès
Publikováno v:
Marine Geology
Marine Geology, Elsevier, 2020, 421, pp.106090. ⟨10.1016/j.margeo.2019.106090⟩
Marine Geology, 2020, 421, pp.106090. ⟨10.1016/j.margeo.2019.106090⟩
Marine Geology, Elsevier, 2020, 421, pp.106090. ⟨10.1016/j.margeo.2019.106090⟩
Marine Geology, 2020, 421, pp.106090. ⟨10.1016/j.margeo.2019.106090⟩
Provenance determination of late Eocene to Quaternary sediments deposited at the DSDP 25 Site 242 may help to evaluate the mechanisms that have controlled the sediment deposition in the Mozambique Channel. To determine the provenance of the clay frac
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::5b58ded80329142744207b58d02916c6
https://doi.org/10.1016/j.margeo.2019.106090
https://doi.org/10.1016/j.margeo.2019.106090