Zobrazeno 1 - 10
of 23
pro vyhledávání: '"Christoph F. Hieronymus"'
Autor:
Mohsen Bazargan, Bjarne S. G. Almqvist, Hem Bahadur Motra, Pooyan Broumand, Tobias Schmiedel, Christoph F. Hieronymus
Publikováno v:
Resources, Vol 11, Iss 5, p 49 (2022)
Laboratory-based elastic wave measurements are commonly used to quantify the seismic properties of Earth’s crust and upper mantle. Different types of laboratory apparatuses are available for such measurements, simulating seismic properties at diffe
Externí odkaz:
https://doaj.org/article/03665a350cf4476a8782ca90ed320cd9
Publikováno v:
Geophysical Journal International. 226:709-727
This article has been accepted for publication in Geophysical Journal International ©: 2021 Vachon, REC, Bazargan, Hieronymus, Ronchin, Almqvist B. Published by Oxford University Press on behalf of the Royal Astronomical Society. All rights reserved
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::cc8e2bbf314d1cbb884a7636bee9daa6
https://doi.org/10.1093/gji/ggab127
https://doi.org/10.1093/gji/ggab127
Publikováno v:
Geophysical Journal International. 218:773-786
Magmas and other viscously deforming fluids in the Earth frequently contain embedded crystals or other solid inclusions. These inclusions generally rotate about their own axis and, under certain co ...
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::6b5be0d21e7eaf16cbd8a5a481feb61b
https://doi.org/10.1093/gji/ggz174
https://doi.org/10.1093/gji/ggz174
Pressure and temperature change simultaneously in the Earth’s crust from surface to depth. Joint pressure and temperature changes influence many different physical properties. There are many studies on samples at elevated pressure, where the influe
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::9c044cdd09fe783fa7d6458f61edddfa
http://urn.kb.se/resolve?urn=urn:nbn:se:uu:diva-457620
http://urn.kb.se/resolve?urn=urn:nbn:se:uu:diva-457620
Autor:
Tobias Schmiedel, Tobias Mattsson, Steffi Burchardt, Christoph F. Hieronymus, Erika Ronchin, Abigail K. Barker, D. W. McGarvie, Emma Rhodes, S. N. Rousku, T. Witcher
Knut och Alice Wallenbergs Stiftelse (Knut and Alice Wallenberg Foundation). Grant Number: KAW 2017.0153 Royal Swedish Academy of Sciences (KVA). Grant Number: GS2019–0024 Center of Natural Hazards and Disaster Science. Although it is widely accept
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::4757f9d6ff51802006dc23885f65d0d1
http://urn.kb.se/resolve?urn=urn:nbn:se:uu:diva-461136
http://urn.kb.se/resolve?urn=urn:nbn:se:uu:diva-461136
As a petrofabric indicator, anisotropy of magnetic susceptibility (AMS) can potentially be used to infer seismic properties of rocks, and in particular seismic anisotropy. To evaluate the link between AMS and seismic anisotropy we present laboratory
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::eae990343f6a7da6934626ee377210e1
http://urn.kb.se/resolve?urn=urn:nbn:se:uu:diva-457616
http://urn.kb.se/resolve?urn=urn:nbn:se:uu:diva-457616
Seismic anisotropy is a key property to understand the structure of the crust and mantle. In this contribution, we investigate the influence of shape (morphological) preferred orientation (SPO), crystallographic preferred orientation (CPO) and the sp
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::0cfea93dbd543834c2e40698e77881a2
https://doi.org/10.5194/egusphere-egu2020-10671
https://doi.org/10.5194/egusphere-egu2020-10671
Autor:
Mohsen Bazargan, Sandra Piazolo, Hem Bahadur Motra, Christoph F. Hieronymus, P. Broumand, Bjarne Almqvist
Publikováno v:
Mineral Exploration Symposium.
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::cb62fe02387f56ca94533336bcd7a4ba
https://doi.org/10.3997/2214-4609.202089023
https://doi.org/10.3997/2214-4609.202089023
Autor:
Christoph F. Hieronymus, Remi Vachon
The dynamics of dyke emplacement are typically modelled by assuming an elastic rheology for the host rock. However, the resulting stress field predicts significant shear failure in the region surrounding the dyke tip. Here, we model the dyking proces
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::0fce681e2cca0f04a718af4527bece21
http://urn.kb.se/resolve?urn=urn:nbn:se:uu:diva-400007
http://urn.kb.se/resolve?urn=urn:nbn:se:uu:diva-400007
Autor:
Christoph F. Hieronymus, Remi Vachon
Publikováno v:
Geophysical Journal International. 208:1414-1429
The size and thickness of dykes is of fundamental importance for volcano dynamics because dykes are the primary path for magma transport, and because large numbers of dykes often comprise a major proportion of the volcanic edifice and of the underlyi
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::33b2c9e3bcdfde428570e50729ade8ed
https://doi.org/10.1093/gji/ggw448
https://doi.org/10.1093/gji/ggw448