Zobrazeno 1 - 10
of 68
pro vyhledávání: '"Andrew McCaig"'
Publikováno v:
Scientific Drilling, Iss 15, Pp 31-35 (2013)
Integrated Ocean Drilling Program (IODP) Expedition 340T returned to the 1.4-km-deep Hole U1309D at Atlantis Massif to carry out borehole logging including vertical seismic profiling (VSP). Seismic, resistivity, and temperature logs were obtained thr
Externí odkaz:
https://doaj.org/article/cd5b8843df934f25a10446a5f96157ce
Autor:
Scott A. Whattam, Gretchen L. Früh-Green, Mathilde Cannat, Jan C.M. De Hoog, Esther M. Schwarzenbach, Javier Escartin, Barbara E. John, Mathew I. Leybourne, Morgan J. Williams, Stéphane Rouméjon, Norikatsu Akizawa, Chiara Boschi, Michelle Harris, Kirsten Wenzel, Andrew McCaig, Dominique Weis, Laura Bilenker
Publikováno v:
Chemical geology 594 (2022). doi:10.1016/j.chemgeo.2021.120681
info:cnr-pdr/source/autori:Whattam S.A.[1], Früh-Green G.L.[2], Cannat M.[3], De Hoog J.C.M.[4], Schwarzenbach E.M.[5], Escartin J.[6], John B.E.[7], Leybourne M.I.[8], Williams M.J.[9], Rouméjon S.[2], Akizawa N.[10], Boschi C.[11], Harris M.[12], Wenzel K.[13], McCaig A.[14], Weis D.[15], Bilenker L.[16]/titolo:Geochemistry of serpentinized and multiphase altered Atlantis Massif peridotites (IODP Expedition 357): Petrogenesis and discrimination of melt-rock vs. fluid-rock processes/doi:10.1016%2Fj.chemgeo.2021.120681/rivista:Chemical geology/anno:2022/pagina_da:/pagina_a:/intervallo_pagine:/volume:594
Whattam, S A, Früh-green, G L, Cannat, M, De Hoog, J C M, Schwarzenbach, E M, Escartin, J, John, B E, Leybourne, M I, Williams, M J, Rouméjon, S, Akizawa, N, Boschi, C, Harris, M, Wenzel, K, Mccaig, A, Weis, D & Bilenker, L 2021, ' Geochemistry of serpentinized and multiphase altered Atlantis Massif peridotites (IODP Expedition 357): Petrogenesis and discrimination of melt-rock vs. fluid-rock processes ', Chemical Geology . https://doi.org/10.1016/j.chemgeo.2021.120681
Chemical Geology, 594
info:cnr-pdr/source/autori:Whattam S.A.[1], Früh-Green G.L.[2], Cannat M.[3], De Hoog J.C.M.[4], Schwarzenbach E.M.[5], Escartin J.[6], John B.E.[7], Leybourne M.I.[8], Williams M.J.[9], Rouméjon S.[2], Akizawa N.[10], Boschi C.[11], Harris M.[12], Wenzel K.[13], McCaig A.[14], Weis D.[15], Bilenker L.[16]/titolo:Geochemistry of serpentinized and multiphase altered Atlantis Massif peridotites (IODP Expedition 357): Petrogenesis and discrimination of melt-rock vs. fluid-rock processes/doi:10.1016%2Fj.chemgeo.2021.120681/rivista:Chemical geology/anno:2022/pagina_da:/pagina_a:/intervallo_pagine:/volume:594
Whattam, S A, Früh-green, G L, Cannat, M, De Hoog, J C M, Schwarzenbach, E M, Escartin, J, John, B E, Leybourne, M I, Williams, M J, Rouméjon, S, Akizawa, N, Boschi, C, Harris, M, Wenzel, K, Mccaig, A, Weis, D & Bilenker, L 2021, ' Geochemistry of serpentinized and multiphase altered Atlantis Massif peridotites (IODP Expedition 357): Petrogenesis and discrimination of melt-rock vs. fluid-rock processes ', Chemical Geology . https://doi.org/10.1016/j.chemgeo.2021.120681
Chemical Geology, 594
International Ocean Discovery Program (IODP) Expedition 357 drilled 17 shallow sites distributed ~10 km in the spreading direction (from west to east) across the Atlantis Massif oceanic core complex (Mid-Atlantic Ridge, 30°N). Mantle exposed in the
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::40c118812ebac27a8f1f457abb54d52e
http://www.cnr.it/prodotto/i/466258
http://www.cnr.it/prodotto/i/466258
The shapes and directionality of bathymetry at slow-spreading ridges are key to understanding the magmatic or tectonic emplacement of the crust. Magmatic terrain is marked by linearly fault-bounded...
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::3c5206429d0496adc2876accd533173c
https://doi.org/10.1002/essoar.10502634.1
https://doi.org/10.1002/essoar.10502634.1
Terrain classification at slow-spreading ridges has been a topic of interest since the significant discovery of mantle rocks exhumed by detachment faults in various segments of the Mid-Atlantic spreading axis. These rocks commonly form domed massifs,
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::7eca8b82367ac815840ee55b336791cb
https://doi.org/10.5194/egusphere-egu2020-337
https://doi.org/10.5194/egusphere-egu2020-337
Autor:
Andrew McCaig, Samuele Agostini, David Banks, Ivan P. Savov, Robert A. Cliff, Sofya Titarenko, Adrian J. Boyce
Publikováno v:
Nature Communications, Vol 9, Iss 1, Pp 1-10 (2018)
Nature Communications
Nature communications 9 (2018). doi:10.1038/s41467-018-07064-6
info:cnr-pdr/source/autori:McCaig A.M.[1], Titarenko S.S.[1], Savov I.P.[1], Cliff R.A.[1], Banks D.[1], Boyce A.[2], Agostini S.[3]/titolo:No significant boron in the hydrated mantle of most subducting slabs/doi:10.1038%2Fs41467-018-07064-6/rivista:Nature communications/anno:2018/pagina_da:/pagina_a:/intervallo_pagine:/volume:9
Nature Communications
Nature communications 9 (2018). doi:10.1038/s41467-018-07064-6
info:cnr-pdr/source/autori:McCaig A.M.[1], Titarenko S.S.[1], Savov I.P.[1], Cliff R.A.[1], Banks D.[1], Boyce A.[2], Agostini S.[3]/titolo:No significant boron in the hydrated mantle of most subducting slabs/doi:10.1038%2Fs41467-018-07064-6/rivista:Nature communications/anno:2018/pagina_da:/pagina_a:/intervallo_pagine:/volume:9
Boron has become the principle proxy for the release of seawater-derived fluids into arc volcanics, linked to cross-arc variations in boron content and isotopic ratio. Because all ocean floor serpentinites so far analysed are strongly enriched in bor
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::7a0c25a6171f90bb13034301c9331b8b
http://link.springer.com/article/10.1038/s41467-018-07064-6
http://link.springer.com/article/10.1038/s41467-018-07064-6
Autor:
Howard Nicholls, Andrew McCaig, James Norcliffe, Estelle Mortimer, David van der Spuy, Douglas A. Paton, Karyna Rodriguez, Neil Hodgson
Seaward Dipping Reflectors (SDRs) are a characteristic feature of magma-rich margins, and represent the generation of large volumes of flood basalts at the point of continental breakup. A number of recent studies provide new insights into the emplace
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::6c028e8e2f7c0da18ee4d34b54e147db
https://eprints.whiterose.ac.uk/137078/1/Norcliffe_et_al_2018.pdf
https://eprints.whiterose.ac.uk/137078/1/Norcliffe_et_al_2018.pdf
Autor:
Andrew McCaig, V. Prasannakumar
Publikováno v:
Journal of the Geological Society of India. 88:421-432
Shear markers and shear sense indicators from the Bhavani shear zone, a member of the shear system separating the northern Archaean and southern Pan African granulite terranes of the South Indian shield, with differently exhumed crustal blocks, sugge
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::4e1119c6855bdb7c766ce205c013b4ad
https://doi.org/10.1007/s12594-016-0505-7
https://doi.org/10.1007/s12594-016-0505-7
Publikováno v:
Philosophical Transactions of the Royal Society A: Mathematical, Physical and Engineering Sciences. 378:20190332
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::ab33d25df5d9307c645d3cb3d2500d6a
https://doi.org/10.1098/rsta.2019.0332
https://doi.org/10.1098/rsta.2019.0332
In recent years it has been recognised that parts of slow spreading ridges such as the Mid-Atlantic Ridge (MAR) are characterised by typical magmatic spreading, while other parts are characterised ...
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::64a1ef72c911dfdb7ef9785310b59fae
https://doi.org/10.1002/essoar.b12d8307abbb5559.c5bea437c8604573.1
https://doi.org/10.1002/essoar.b12d8307abbb5559.c5bea437c8604573.1
Autor:
Andrew McCaig, Sofya Titarenko
Publikováno v:
Geofluids. 16:314-328
The Lost City hydrothermal field (LCHF) is hosted in serpentinite at the crest of the Atlantis Massif, an oceanic core complex close to the mid-Atlantic Ridge. It is remarkable for its longevity and for venting low-temperature (40–91°C) alkaline f
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::0a18ccdc55969d5ad84074e7cdf47ebf
https://doi.org/10.1111/gfl.12151
https://doi.org/10.1111/gfl.12151