Zobrazeno 1 - 10
of 31
pro vyhledávání: '"Miguel J. Haller"'
Publikováno v:
Boletín Geográfico, Vol 43, Iss 1 (2021)
El análisis morfométrico de los conos de escoria permite evaluar los procesos erosivos que los afectan e inferir la historia eruptiva de una región. Utilizando DEMs TanDEM-X de 12 m de resolución se midieron los parámetros morfológicos de 157 c
Externí odkaz:
https://doaj.org/article/9e296ffc22e94f10b7d8d2f949a4bdb6
Autor:
Pierre‐Arnaud Desiage, Guillaume St‐Onge, Mathieu J. Duchesne, Jean‐Carlos Montero‐Serrano, Miguel J. Haller
Publikováno v:
Journal of Quaternary Science.
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::4af0235c3ecf5959144fc2f5d3e425ac
https://doi.org/10.1002/jqs.3511
https://doi.org/10.1002/jqs.3511
Autor:
Miguel J. Haller, Gabriela Isabel Massaferro, Paul Martin Holm, Nina Søager, Marie Katrine Traun
Publikováno v:
Gondwana Research. 91:40-57
Based on an extensive literature dataset on Cenozoic intraplate basalts from Patagonia, Argentina, we provide a revised interpretation of the mantle sources of volcanism and suggest a relation to the South Atlantic hotspots and mantle flow. Furthermo
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::1a245c0057d7ce390cf70576b20262b0
https://doi.org/10.1016/j.gr.2020.12.008
https://doi.org/10.1016/j.gr.2020.12.008
Autor:
Gloria Gallastegui, Claudia Beatriz Zaffarana, Víctor Ruiz González, Stella Poma, Diego G. Silva Nieto, Darío Leandro Orts, Miguel J. Haller, Gerhard Wörner, Bárbara Boltshauser, Raúl Eduardo Giacosa, Carla G. Puigdomenech Negre, Alicia Busteros, Silvia Lagorio, Daniel Alfredo Gregori
Publikováno v:
RID-UNRN (UNRN)
Universidad Nacional de Río Negro
instacron:UNRN
Universidad Nacional de Río Negro
instacron:UNRN
Fil: Zaffarana, Claudia B. Consejo Nacional de Investigaciones Científicas y Técnicas. Buenos Aires, Argentina. Fil: Lagorio, Silvia L. Servicio Geológico y Minero Argentino (SEGEMAR). Buenos Aires, Argentina. Fil: Gallastegui, Gloria. Instituto G
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::27619d163d42743a100ebda4e5608d26
http://rid.unrn.edu.ar/handle/20.500.12049/5424
http://rid.unrn.edu.ar/handle/20.500.12049/5424
Publikováno v:
Quaternary of South America and Antarctic Peninsula
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::ebd37aaedcce7079be802869797294cc
https://doi.org/10.1201/9781003079484-13
https://doi.org/10.1201/9781003079484-13
Autor:
Nilda Menegatti, Miguel J. Haller, Viviana Ines Alric, Gabriela Isabel Massaferro, César Navarrete
Publikováno v:
Journal of South American Earth Sciences. 102:102650
During Cenozoic times, Patagonia was characterized by an intense magmatic intraplate activity that gave rise to a large volume of basaltic flows and intrusive bodies. This work aims to gather all the available information along with unpublished data
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::4422c13cf580ea238107a7e60a5c282b
https://doi.org/10.1016/j.jsames.2020.102650
https://doi.org/10.1016/j.jsames.2020.102650
Autor:
Monica Noemi Gil, Miguel J. Haller, Guillaume St-Onge, Erica Giarratano, Augusto César Crespi-Abril, Pierre-Arnaud Desiage, Jean-Carlos Montero-Serrano
Publikováno v:
CONICET Digital (CONICET)
Consejo Nacional de Investigaciones Científicas y Técnicas
instacron:CONICET
Consejo Nacional de Investigaciones Científicas y Técnicas
instacron:CONICET
The Gulf of San Jorge (GSJ) is a semicircular basin, approximately 160 km long and 250 km wide, located in the central part of Patagonia between 45°S and 47°S, lacking any present-day major perennial tributaries. The grain size and bulk and clay mi
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::1f6eb9b4fe8d57c3492485a9d6b817c6
https://tos.org/oceanography/article/quantifying-sources-and-transport-pathways-of-surface-sediments-in-the-gulf
https://tos.org/oceanography/article/quantifying-sources-and-transport-pathways-of-surface-sediments-in-the-gulf
Autor:
Carla G. Puigdomenech Negre, Alicia Busteros, Miguel J. Haller, Víctor Ruiz González, Darío Leandro Orts, Diego G. Silva Nieto, Bárbara Boltshauser, Rubén Somoza, Raúl Eduardo Giacosa, Silvia Lagorio, Claudia Beatriz Zaffarana
Publikováno v:
RID-UNRN (UNRN)
Universidad Nacional de Río Negro
instacron:UNRN
Universidad Nacional de Río Negro
instacron:UNRN
Fil: Zaffarana, Claudia B. Consejo Nacional de Investigaciones Científicas y Técnicas. Buenos Aires, Argentina. Fil: Lagorio, Silvia L. Servicio Geológico Minero Argentino (SEGEMAR). Buenos Aires, Argentina. Fil: Orts, Darío L. Consejo Nacional d
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::a9f0e9d8fd6e082c6a33c17a32e65027
http://rid.unrn.edu.ar/handle/20.500.12049/5423
http://rid.unrn.edu.ar/handle/20.500.12049/5423
Autor:
Miguel J. Haller
Publikováno v:
Late Cenozoic of Península Valdés, Patagonia, Argentina ISBN: 9783319485072
Late Cenozoic of Península Valdés, Patagonia, Argentina
Late Cenozoic of Península Valdés, Patagonia, Argentina
The surface of Península Valdés is gently cut, characterized by plateaus, sea cliffs, and spits as well as depressions caused by a complex process of tectonic, deflation, fluvial erosion, and mass wasting. Subsurface geology comprises early Paleozo
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::5771ded554a4e48d9799e91be1b02b5c
https://doi.org/10.1007/978-3-319-48508-9_2
https://doi.org/10.1007/978-3-319-48508-9_2
Publikováno v:
Journal of Volcanology and Geothermal Research. 201:253-271
The morphologic parameters, pyroclastic deposits and evolution of maar–diatreme volcanoes are affected by the type of environment in which they are emplaced. End-member cases are a hard substrate (rocks) and a soft substrate (unconsolidated volcani
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::2e3c882036b595dd518f8f89f9456505
https://doi.org/10.1016/j.jvolgeores.2010.07.018
https://doi.org/10.1016/j.jvolgeores.2010.07.018