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pro vyhledávání: '"F. Martineau"'
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Autor:
Kenji Watanabe, D Pham, O. Ndoye, F Martineau, Christophe Chevalier, C. Minatchy, F Szymkiewicz, V Vidal, F Lachaussée
Publikováno v:
Scopus-Elsevier
Overflow erosion has been mostly studied on cohesionless model dike and with an initial breach. Very few studies concern cohesive embankment because there is neither a standard material nor a shared protocol. Dealing with erosion of cohesive soils al
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::f4b7935bb7f32a55c2902f2a6d059ab8
https://doi.org/10.1201/9781315375045-80
https://doi.org/10.1201/9781315375045-80
Autor:
David F. Martineau
Publikováno v:
AAPG Bulletin. 91:399-403
David Martineau is a certified petroleum geologist and received his B.S. degree in geology from the University of Texas in 1960. He joined Pitts in 1972 and is the exploration manager. Pitts has been involved in the Barnett play since its inception.
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::957fc1fb33512b4c6a1623366f264878
https://doi.org/10.1306/intro910407
https://doi.org/10.1306/intro910407
Autor:
F Martineau, Serge Fourcade, M Ayt Ougougdal, Michel Cathelineau, Alain Trouiller, Etienne Deloule, Stéphane Buschaert
Publikováno v:
Applied Geochemistry. 19:1201-1215
Mesozoic limestones from the eastern part of the Paris Basin display, mostly in strata rich in bioherms, abundant macro-cavities (vugs) and some connected micro-fractures almost completely filled with euhedral calcite crystals (late calcite spar). Th
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::234b67f09d54b9343d362badde169b94
https://doi.org/10.1016/j.apgeochem.2003.01.001
https://doi.org/10.1016/j.apgeochem.2003.01.001
Autor:
Sidonie Révillon, Catherine Chauvel, Nicholas Arndt, R Pik, Serge Fourcade, F Martineau, Bernard Marty
Publikováno v:
Earth and Planetary Science Letters. 205:91-106
The composition of the mantle plumes that created large oceanic plateaus such as Ontong Java or the Caribbean is still poorly known. Geochemical and isotopic studies on accreted portions of the Caribbean plateau have shown that the plume source was h
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::9773cb706fee99cda9fa322b2a059074
https://doi.org/10.1016/s0012-821x(02)01003-8
https://doi.org/10.1016/s0012-821x(02)01003-8
Publikováno v:
Lithos. 59:171-198
In NE China, voluminous granitoids were emplaced in late Paleozoic and Mesozoic times. We report here Sr–Nd–O isotopic and elemental abundance data for two highly evolved granitic plutons, Woduhe and Baerzhe, from the Great Xing'an Mountains. The
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::588bfbff10c2c755a8914bd47dd0bb5f
https://doi.org/10.1016/s0024-4937(01)00066-4
https://doi.org/10.1016/s0024-4937(01)00066-4
Autor:
Marie-Christine Boiron, Serge Fourcade, Michel Cathelineau, F. Martineau, Cécile Fabre, Christian Marignac, Jean Vallance
Publikováno v:
Tectonophysics. 336:43-61
The Vaulry W–(Sn) mineralisation, located at the eastern boundary of the Blond rare metal leucogranite, is contained in a set of subvertical quartz veins, locally with muscovite and minor quartz selvages. The sequence of deposition was: (1) milky q
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::3f0031270abcf290dfc00079baa24548
https://doi.org/10.1016/s0040-1951(01)00093-2
https://doi.org/10.1016/s0040-1951(01)00093-2
Publikováno v:
Lithos. 57:187-216
In northern Algeria, the coastal area displays a very variegated magmatism of Miocene age, extending E–W over 900 km with a width of less than 50 km. This magmatism includes both plutonic and volcanic massifs containing basic, intermediate to acidi
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::b200eedc854e0aaafdcaa8f142887ea3
https://doi.org/10.1016/s0024-4937(01)00034-2
https://doi.org/10.1016/s0024-4937(01)00034-2
Publikováno v:
Chemical Geology. 168:211-223
In the the Armorican Massif (NW France), the formation of kaolinite in surficial conditions is demonstrated by the existence of alteration profiles enriched in kaolinite at the top of metamorphic and sedimentary formations. For some of the largest de
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::d70bcb5acd059ab176094b805fb41bcb
https://doi.org/10.1016/s0009-2541(00)00225-4
https://doi.org/10.1016/s0009-2541(00)00225-4
Publikováno v:
Journal of Geochemical Exploration. :561-564
During post-thickening extensional collapse, deformation can be localised within flat-lying decollement zones where fluids are present. General questions concern the nature and origin of fluids, the scale of their transfer, and the coupling between s
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::df9852b5c2d5c12706135cf3242dd437
https://doi.org/10.1016/s0375-6742(00)00121-7
https://doi.org/10.1016/s0375-6742(00)00121-7