Zobrazeno 1 - 10
of 34
pro vyhledávání: '"Alexey Shulgin"'
The western edge of the Baltic Shield is covered by the northeast – southwest oriented, 2500 m high mountain range, the Scandes at the northwestern Atlantic Ocean. This mountain range is located far from any active plate boundary and lack of sedime
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::6696ef303f264572fe184d1ecc56188c
https://doi.org/10.5194/egusphere-egu23-15239
https://doi.org/10.5194/egusphere-egu23-15239
Autor:
Alexey Shulgin, Irina Artemieva
We present a joint continental-oceanic upper mantle density model based on 3D tesseroid gravity modeling. On continent lithospheric mantle (LM) density shows no clear difference between the cratonic and Phanerozoic Europe, yet an ~300‐km‐wide zon
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::8a656bdcbcde4ee2e9a4908e909435c0
https://doi.org/10.5194/egusphere-egu23-6967
https://doi.org/10.5194/egusphere-egu23-6967
Autor:
Rafet Ender Alemdar, Metin Kahraman, Alexey Shulgin, Rolf Mjelde, Irina Artemieva, Hans Thybo
The Senja onshore-offshore seismic profile is located in the north-western part of Europe across the Norwegian coast into the North Atlantic ocean. A number of terranes and microcontinents collided to form this region from the Archean to the Paleopro
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::029042711ef09fe190ef5e254ed6ac31
https://doi.org/10.5194/egusphere-egu23-15662
https://doi.org/10.5194/egusphere-egu23-15662
Autor:
Alexey Shulgin, Irina Artemieva
We present a new model for the density structure of the lithospheric upper mantle beneath the Siberian craton, based on a 3D tesseroid gravity modeling. Our model is based on a detailed crustal structural database SibCrust (Cherepanova et al., 2013)
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::7302ebe8c0818457609638d514b8f55d
https://doi.org/10.5194/egusphere-egu22-5771
https://doi.org/10.5194/egusphere-egu22-5771
The Baltic Shield is located in the northern part of Europe. It formed by amalgamation of a series of terranes and microcontinents during the Archean to the Paleoproterozoic, followed by significant modification in Neoproterozoic to Paleozoic time by
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::612c0a031627f9edaec1f8d7bdae726e
https://doi.org/10.5194/egusphere-egu22-3139
https://doi.org/10.5194/egusphere-egu22-3139
Autor:
Irina M. Artemieva, Alexey Shulgin
Publikováno v:
Tectonics. 38:4465-4487
We present the first thermal model for the lithosphere in Turkey, which shows a highly heterogeneous pattern associated with mosaics of the Tethyan and modern subduction systems. We calculate a regionally average crustal density of 2.90 g/cm3 consist
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::c9624b80039cfff469c2977872d9da43
https://doi.org/10.1029/2019tc005594
https://doi.org/10.1029/2019tc005594
Autor:
Alexey Shulgin, Irina M. Artemieva
Knowledge of the crustal structure is the key for understanding physical and chemical conditions of its formation and later modification by geodynamic processes. It has long been recognized that crustal structure is controlled by tectonic settings, a
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::28faf142cac567c806b759f289156043
https://doi.org/10.1111/1755-6724.14829
https://doi.org/10.1111/1755-6724.14829
Autor:
Irina M. Artemieva, Alexey Shulgin
Publikováno v:
Journal of Geophysical Research: Solid Earth. 124:9280-9312
We present a new model, EUNA‐rho, for the density structure of the continental and oceanic upper mantle based on 3‐D tesseroid gravity modeling. On continent, there is no clear difference in lithospheric mantle (LM) density between the cratonic a
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::275f737060d66ccadbda30dd192855cc
https://doi.org/10.1029/2018jb017025
https://doi.org/10.1029/2018jb017025
Autor:
Irina M. Artemieva, Alexey Shulgin
Publikováno v:
Earth and Planetary Science Letters. 512:8-16
Crustal structure preserves a unique record of physical and chemical conditions of its formation and later modification by geodynamic processes. The existence of broad global correlations between crustal structure and tectonic settings led to models
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::445dc1a91d8dfc50e27bb60fd9598d35
https://doi.org/10.1016/j.epsl.2019.01.033
https://doi.org/10.1016/j.epsl.2019.01.033
The Baltic Shield is located in the northern part of Europe, which formed by amalgamation of a series of terranes and microcontinents during the Archean to the Paleoproterozoic, followed by significant modification in Neoproterozoic to Paleozoic time
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::b82157bd1e9129043e51ac0937548b63
https://doi.org/10.5194/egusphere-egu21-15666
https://doi.org/10.5194/egusphere-egu21-15666