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Rift and Rifted Margins Online Seminar
Приєднався 15 чер 2020
This monthly online seminar is currently organised by Sascha Brune (GFZ), J. Kim Welford (Memorial University of Newfoundland), Folarin Kolawole (Columbia University, New York), Derek Keir (Univ. of Florence), Gwenn Péron-Pinvidic (NTNU Trondheim) and Lydia Olaka (Technical University of Kenya). Earlier sessions have been co-organized by Gianreto Manatschal (Univ. Strasbourg), Susanne Buiter (RWTH Aachen), Giacomo Corti (Univ. Florence), Lucia Perez-Diaz (Halliburton & Oxford Univ.) and Rebecca Bell (Imperial College London).
Upcoming sessions are listed here: www.gfz-potsdam.de/index.php?id=10845
Upcoming sessions are listed here: www.gfz-potsdam.de/index.php?id=10845
74.3 Romain Corseri - Magnetotelluric investigations of rifted systems
74.3 Romain Corseri - Magnetotelluric investigations of rifted systems
Переглядів: 51
Відео
74.2 Luise Dambly - Magnetotelluric investigation of rifting and geothermal resources in Ethiopia
Переглядів 739 годин тому
74.2 Luise Dambly - Magnetotelluric investigation of rifting and geothermal resources in Ethiopia
74.1 Kate Selway - Magnetotelluric imaging of the East African Rift and Northern Tanzania Divergence
Переглядів 1869 годин тому
74.1 Kate Selway - Magnetotelluric imaging of the East African Rift and Northern Tanzania Divergence
73.3 Thomas Theunissen - Tectonics and surface processes during oblique rifted margin formation
Переглядів 72Місяць тому
73.3 Thomas Theunissen - Tectonics and surface processes during oblique rifted margin formation
73.2 Jie Chen - 3-D seismic tomography of the oblique north-eastern Gulf of Aden continental margin
Переглядів 75Місяць тому
73.2 Jie Chen - 3-D seismic tomography of the oblique north-eastern Gulf of Aden continental margin
73.1 Elisabetta Panza - Rift obliquity in the Northern Volcanic Zone in Iceland using UAV data
Переглядів 119Місяць тому
73.1 Elisabetta Panza - Rift obliquity in the Northern Volcanic Zone in Iceland using UAV data
72.3 Armagan Kaykun - Structural evolution of Black Sea Basin using sectioned computational models
Переглядів 285Місяць тому
72.3 Armagan Kaykun - Structural evolution of Black Sea Basin using sectioned computational models
72.2 Helene-Sophie Hilbert - From symmetric to asymmetric spreading: Central Mariana Trough
Переглядів 83Місяць тому
72.2 Helene-Sophie Hilbert - From symmetric to asymmetric spreading: Central Mariana Trough
72.1 Geoffroy Mohn - Breakup of marginal seas and differences from Atlantic type margins
Переглядів 123Місяць тому
72.1 Geoffroy Mohn - Breakup of marginal seas and differences from Atlantic type margins
71.3 Erica Lucas - Impact of regional scale mantle structure beneath the West Antarctic Rift System
Переглядів 864 місяці тому
71.3 Erica Lucas - Impact of regional scale mantle structure beneath the West Antarctic Rift System
71.2 Valentin Rime - Flooding of the Danakil rift basin (Afar, Ethiopia)
Переглядів 2144 місяці тому
71.2 Valentin Rime - Flooding of the Danakil rift basin (Afar, Ethiopia)
71.1 Lisa McNeill - High rates of Corinth Rift (Greece) extension and sea level interactions
Переглядів 1224 місяці тому
71.1 Lisa McNeill - High rates of Corinth Rift (Greece) extension and sea level interactions
70.1 Paul Olsen - Drilling continental rift basins on the eastern North American margin
Переглядів 1035 місяців тому
70.1 Paul Olsen - Drilling continental rift basins on the eastern North American margin
70.3 Anneleen Foubert - Afar Dallol Drilling as key to unlock complexity of rifts and rifted margins
Переглядів 1125 місяців тому
70.3 Anneleen Foubert - Afar Dallol Drilling as key to unlock complexity of rifts and rifted margins
70.2 Joann Stock - Drilling into the South China Sea
Переглядів 835 місяців тому
70.2 Joann Stock - Drilling into the South China Sea
69.2 Erin DiMaggio - Highres geologic mapping and tephrochronology of Ledi-Geraru site, Ethiopia
Переглядів 2366 місяців тому
69.2 Erin DiMaggio - Highres geologic mapping and tephrochronology of Ledi-Geraru site, Ethiopia
69.3 Lindsay McHenry - Olduvai basin and its often rift-controlled paleolake
Переглядів 1506 місяців тому
69.3 Lindsay McHenry - Olduvai basin and its often rift-controlled paleolake
69.1 Céline Marie Vidal - Volcanic ash in the East African Rift: Origins and applications
Переглядів 1856 місяців тому
69.1 Céline Marie Vidal - Volcanic ash in the East African Rift: Origins and applications
68.3 Sudipta Tapan Sinha - Stretching buoyancy interplay in the magma-poor rifting process
Переглядів 637 місяців тому
68.3 Sudipta Tapan Sinha - Stretching buoyancy interplay in the magma-poor rifting process
68.2 Anindita Samsu - Structural inheritance in amagmatic rift basins: the norm, not the exception?
Переглядів 1567 місяців тому
68.2 Anindita Samsu - Structural inheritance in amagmatic rift basins: the norm, not the exception?
68.1 Rasheed Ajala - Blind magmatism abets nonvolcanic continental rifting
Переглядів 1817 місяців тому
68.1 Rasheed Ajala - Blind magmatism abets nonvolcanic continental rifting
67.3 Gabriel Pasquet - Basalt alteration and natural hydrogen geothermal synergies in Djibouti
Переглядів 1758 місяців тому
67.3 Gabriel Pasquet - Basalt alteration and natural hydrogen geothermal synergies in Djibouti
67.2 Frank Zwaan - Natural H2 potential in inverted rift basins, shown by numerical models
Переглядів 1688 місяців тому
67.2 Frank Zwaan - Natural H2 potential in inverted rift basins, shown by numerical models
67.1 Z. Liu, M. Pérez-Gussinyé, J. García-Pintado - Mantle serpentinization and associated hydrogen
Переглядів 1768 місяців тому
67.1 Z. Liu, M. Pérez-Gussinyé, J. García-Pintado - Mantle serpentinization and associated hydrogen
66.3 Rūta Karolytė - Isotopic indicators of early continental rifting
Переглядів 1089 місяців тому
66.3 Rūta Karolytė - Isotopic indicators of early continental rifting
66.2 Hanneke Paulssen - A magnitude 6.5 earthquake in Botswana: Rifting of the Kalahari Craton?
Переглядів 1359 місяців тому
66.2 Hanneke Paulssen - A magnitude 6.5 earthquake in Botswana: Rifting of the Kalahari Craton?
66.1 Brian Taylor - Itina Trough: a young rift, not a fossil trench nor fracture zone
Переглядів 1649 місяців тому
66.1 Brian Taylor - Itina Trough: a young rift, not a fossil trench nor fracture zone
65.3 Derek Neuharth - Evolution of rift systems and their faults in response to surface processes
Переглядів 46510 місяців тому
65.3 Derek Neuharth - Evolution of rift systems and their faults in response to surface processes
65.2 Tiphaine Larvet - Slab Pull and Continental Breakup
Переглядів 15810 місяців тому
65.2 Tiphaine Larvet - Slab Pull and Continental Breakup
65.1 Ritske Huismans - 3D Large Deformation Forward Modeling of Crust and Lithosphere Extension
Переглядів 11910 місяців тому
65.1 Ritske Huismans - 3D Large Deformation Forward Modeling of Crust and Lithosphere Extension
UA-cam when you go to hell take your advertisers with you!
that's my dad
Thanks for the lesson. It's interesting how seas have obscured so many dynamically tectonic areas. Now I wonder. What might the Caspian be shrouding?
The North American plate mid-continental rift was from large long meteorite string of pearl impacts causing significant volcanism never having the continent split in two to be why it's oddly linearly disconnected to be a very important World War Meteorite Age scientific research case study.
Interesting video but I wish it had gone into more detail. An hour-long presentation (or even longer) would have been better IMO.
Wonderful. Amazing data!
Great presentation! Do you think slab pull was involved with the breakup of the last supercontinent Pangea. I was just reading some research that suggest there was westward subduction on the pacific coast as the exotic terranes were being accreted.
Where are blues from, miles Davis
Great to see you, Rasheed. Great work
Ta the video. This rift arm extends SW into Namibia parallel and outboard of the NeoProterozoic Damara Belt/PalaeoProterozoic Kaalhari Belt contact. It is bounded in the north by the Gomare Fault, just south of Gam. Depths of the Kalahari Group sediments increase from about one to several hundred meters across the northern rift edge, with coarse alluvial clastic and lacustrine sediments within the trough, and preserved, downfaulted Karoo Supergroup underlying. Africa's coming apart at the seams, so hold on to your seats. All the best from Namibia.
Great presentation! Thx
it is so cool and interesting
I do want to do something , I just dont believe it's physically possible for a man in my condition
great, much interesting and informative talk
Thank you very much, it helped me a lot with the preparation of the seminar paper.
I love your work. I’ve been following it closely and you have done an amazing job. I do have a question. There is a major strike slip fault that runs east to west south of Iberia. Could this be the cause of these larger earthquakes?
great work Rita.
Informative talk, and I learned so much.
A great presentation. My MT was about rifting and crustal oceanization and great to see all these updated info.
Thank you for this, quite insightful professor.
Wow. Fantastic information. Thanks so much.
Thanks Dr Bailey for your excellent presentation. Please did you consider the effect of compaction on your kinematic analysis or is it negligible?
This is in America, please don’t use the damn metric system.
Scientists don’t use imperial Mike.
Florida Man speaks!
We use the metric system in the US military, and only in civi land do we really see a dependence on the Imperial System, so... even in America, we use metrics. 😊
@@paulfidler3710 Base 12 number systems > base 10 number systems. suck it
@@dillan6134 What's the volume of a 1'×1'×1' cube in US customary or imperial units of volume? (Or a 1"×1"×1" one if you prefer.) What's its approximate mass? (From memory and all math done in your head.) In Imperial/US customary the bases (or more properly the conversion factors) depend on what you're measuring, what units you're converting to and from, and where in the world you are. For length it's 12, 3, and 1760 (for both). For volume it's 3, 2, 8, 2, 2, and 4 (US) or 3, 1.6, 10, 2, 2, and 4 (Imperial). For mass it's 16 and 2000 (US) or 16, 14, and 160 (Imperial). And that's just for the common, everyday units. In metric the factor is always a power of 10. That's not even considering the relationship between the different base units (for length, volume, etc.).
very good and concise information
I always watch your informative lectures. Can you please make a lecture about salt tectonics, importance of salt in hydrocarbon exploration. Thanks
I want to learn this.. Please help me.. Although I’m a student, but I can pay some money for learning these. 🙏🥺
Really insightful presentation. Looking forward to the continuation.
Good done
Nice investigation and awesome talk
good talk!
Great work, Pagli.
If you want to contact me regarding this talk, please email me at: gael.lymer@ucd.ie Any question or comment welcome :) Please click "like" if you enjoyed this video.
Thank you for this. Fascinating.
nice talk
Very informative. Thanks a lot for sharing !
SOMALI
These series of seminars are been awesome. Congrats to the everyone involved on it!!!
Great talk Folar
Really great talk, Gary Karner, Thank you very much!
Great research, Clara. It's a lot of hard work you put into this. Thank you.
I love the presentation I very complex system and very well explained. Is a monumental work !! Congratulations!