Waveform inversion of the S reflector west of Spain: fine structure of a detachment fault. [PDF]
, 2005 The S reflection west of Iberia has been interpreted as a low-angle detachment fault separating crustal fault blocks from partially serpentinized mantle. We apply full waveform inversion to investigate the fine structure of S.
Minshull, TA +7 more
core +1 more source
Crustal magmatic controls on the formation of porphyry copper deposits
Nature Reviews Earth & Environment, 2021 Jung-Woo Park +4 more
semanticscholar +1 more source
Crustal structure of the Cape Verde Swell: Insights into the flexural response of the lithosphere to loading [PDF]
, 2011 Throughout the ocean basins many broad regions of anomalously shallow topography exist that do not fit the widely accepted model of conductive plate cooling and subsidence as a function of lithospheric age.
Wilson, Dean James, WILSON, DEAN,JAMES
core
Método do fluxo de massa na avaliação do intemperismo de fontes de contaminação em águas subterrâneas [PDF]
, 2012 TCC(graduação) - Universidade Federal de Santa Catarina. Centro Tecnológico. Engenharia Sanitária e Ambiental.A água subterrânea exerce um papel fundamental na distribuição de água potável para a população.
Cristiano, Djema Maria
core
Análise do índice de contaminação e perfil bacteriológico dos colírios utilizados no dia-a-dia da oftalmologia. [PDF]
, 2009 Trabalho de Conclusão de Curso - Universidade Federal de Santa Catarina. Curso de Medicina.
Nobre, Jayme Quirino Caon
core
Crustal fault reactivation facilitating lithospheric folding/buckling in the central Indian Ocean
, 1996 High-quality, normal-incidence seismic reflection data confirm that tectonic deformation in the central Indian Ocean occurs at two spatial scales: whole lithosphere folding with wavelengths varying between 100 and 300 km, and compressional reactivation ...
Beekman, F. +3 more
core +1 more source
Seismic investigation of crustal accretion at the slow spreading Mid-Atlantic Ridge-The Reykjanes Ridge at 57 45'N [PDF]
, 1996 Studies of mid-ocean ridges have provided evidence of magma chambers beneath both fast and intermediate spreading ridges. However no such features have been observed to date beneath slow spreading ridges.
Navin, D.A.
core
, 2012 [1] The Cameroon Volcanic Line (CVL) in West Africa is a chain of Cenozoic volcanism with no clear age progression. The reasons for its existence are unclear, and the nature of its magmatic plumbing system is poorly understood.
Bastow, I.D., Gallacher, R.J.
core +1 more source
Stationary flux ropes at the southern terminator of Mars [PDF]
, 2012 Flux ropes have long been observed in the upper atmosphere of Venus, and more recently at Mars. Here we present magnetic field measurements of flux ropes encountered at the southern terminator of Mars by Mars Global Surveyor, and compare them to a flux ...
Beharrell, Mat, Wild, James
core +1 more source
Faults, fluids and friction : effect of pressure solution and phyllosilicates on fault slip behaviour, with implications for crustal rheology [PDF]
, 2000 In order to model the mechanics of motion and earthquake generation on large crustal fault zones, a quantitative description of the rheology of fault zones is prerequisite.
IVAU: Instituut voor Aardwetenschappen Utrecht +3 more
core +1 more source