Zobrazeno 1 - 9
of 9
pro vyhledávání: '"Hugues Longuépée"'
Publikováno v:
Minerals, Vol 11, Iss 379, p 379 (2021)
Minerals
Volume 11
Issue 4
Minerals
Volume 11
Issue 4
Glacial drift exploration methods are well established and widely used by mineral industry exploring for blind deposit in northern territories, and rely on the dispersion of mineral or chemical signal in sediments derived from an eroded mineralized s
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::ef86adcc9e6545a492617f661ac806c9
https://www.mdpi.com/2075-163X/11/4/379
https://www.mdpi.com/2075-163X/11/4/379
Publikováno v:
Minerals
Volume 11
Issue 4
Minerals, Vol 11, Iss 337, p 337 (2021)
Volume 11
Issue 4
Minerals, Vol 11, Iss 337, p 337 (2021)
The quantitative and qualitative assessment of gold grains from samples of glacial till is a well-established method for exploring gold deposits hidden under glaciated cover. This method, which is widely used in the industry and has resulted in numer
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::0c7cdf08df30bca434cec50c7ac5facb
Publikováno v:
Journal of Geochemical Exploration. 229:106821
Determining the number of gold grains in till is a widely used exploration technique in glaciated terrain. Nonetheless, there is no existing reference material to assess the quality of either the recovery or the counting of gold particles in samples
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::436f6b0c51ad3a21e6028c27ffa33974
https://doi.org/10.1016/j.gexplo.2021.106821
https://doi.org/10.1016/j.gexplo.2021.106821
Publikováno v:
Geological Society of America Abstracts with Programs.
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::1e69ea73f676d28549c9a24b85752596
https://doi.org/10.1130/abs/2016ne-272769
https://doi.org/10.1130/abs/2016ne-272769
Autor:
Pierre A. Cousineau, Hugues Longuépée
Publikováno v:
The Canadian Mineralogist. 44:967-980
The term glauconite covers a series of iron-rich minerals that form in the upper layer of sediments of the sea bottom in locations where sediment input is low. Because of its potassium content and the process of its formation, it is one of few minera
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::fbd9376bfd1371653418955b72a1e3c2
https://doi.org/10.2113/gscanmin.44.4.967
https://doi.org/10.2113/gscanmin.44.4.967
Autor:
Pierre A. Cousineau, Hugues Longuépée
Publikováno v:
Canadian Journal of Earth Sciences. 42:259-272
The Cambrian Anse Maranda Formation is a glauconite-bearing clastic succession within the Quebec Reentrant. It is part of the Appalachians Humber Zone, particularly of the shale feldspathic sandstone assemblage, which represents the rift-to-drift
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::a34f164fbff0e30cf5ad0f0a5831674a
https://doi.org/10.1139/e05-003
https://doi.org/10.1139/e05-003
Publikováno v:
Journal of Sedimentary Research. 73:217-226
Shoreface sediments exposed in raised deltaic deposits along the Hudson Bay coast are characterized by a thick succession of predominantly parallel-laminated and small-scale cross-laminated fine sand. Ripple forms, where preserved, include both combi
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::d4f955cb0a929de6042e26a47b28d541
https://doi.org/10.1306/080802730217
https://doi.org/10.1306/080802730217
Autor:
Hugues Longuépée, Pierre A. Cousineau
Publikováno v:
Canadian Journal of Earth Sciences. 40:207-219
An improved paleogeography of the Quebec reentrant has been achieved by examining the nature and distribution of major sediment buildups within this reentrant. The Quebec reentrant has one side produced by rift faults and one side by a major transfor
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::263b794cb8237ad37fd2b1799899fc1f
https://doi.org/10.1139/e02-107
https://doi.org/10.1139/e02-107
Autor:
Hugues Longuépée
Publikováno v:
Sédimentation en marge d'un promontoire cambro-ordovicien :: le groupe d'Ile d'Orléans, Appalaches du Québec
La comprehension des chaines orogeniques passe inevitablement par la connaissance de la morphologie des elements qui entrent en collision. La presence de promontoires et reentrants le long de la marge laurentienne a largement influence la distributio
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::b9eca023a71843b6fc5e05a1cc0bbb11
https://doi.org/10.1522/24606931
https://doi.org/10.1522/24606931