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Outer rise stress changes related to the subduction of the Juan Fernandez Ridge, central Chile
(2007)
Although outer rise seismicity is less common than interplate seismicity in subduction zones, a significant level of seismicity has occurred between the Nazca trench and Juan Fernandez Ridge, in central Chile, during the ...
Diseño de un generador trifásico de hundimientos e interrupciones de voltaje AC
(2014)
El propósito de esta Tesis es el desarrollo de un equipo generador trifásico de hundimientos de tensión SAG/DIP e interrupciones de corta duración. Este generador debe producir de manera controlada perturbaciones de ...
PALEOSTRESS FIELDS AND 3-D STRUCTURE OF POLIPHASE SHEAR ZONES IN THE TRANSITION CRATON-OROGENIC BELT: EXAMPLES FROM THE NEOPROTEROZOIC OF SOUTHEASTERN BAHIA, BRAZILPALEOSTRESS FIELDS AND 3-D STRUCTURE OF POLIPHASE SHEAR ZONES IN THE TRANSITION CRATON-OROGENIC BELT: EXAMPLES FROM THE NEOPROTEROZOIC OF SOUTHEASTERN BAHIA, BRAZIL
(Sociedade Brasileira de Geologia, 2017)
Earthquake and tsunami forecasts: Relation of slow slip events to subsequent earthquake rupture
(National Academy of Sciences, 2014-11-17)
The 5 September 2012 Mw 7.6 earthquake on the Costa Rica subduction plate boundary followed a 62-y interseismic period. Highprecision GPS recorded numerous slow slip events (SSEs) in the decade leading up to the earthquake, ...
Paleostress Fields And 3-D Structure Of Poliphase Shear Zones In The Transition Craton-Orogenic Belt: Examples From The Neoproterozoic Of Southeastern Bahia, Brazil
(2000)
The IICSZ is a N45°-trending, 30km wide, intracratonic shear zone, extending for some 150km through the SSE portion of the Bahia State. The IICSZ is closely related to dykes and syenites of the Alkaline Igneous Suite of ...
Geologia do depósito LODE Au-As-Sb Laranjeiras, em metaturbitos do Grupo Nova Lima, Quadrilátero Ferrífero, Minas Gerais, Brasil
(Universidade Federal de Minas GeraisUFMG, 2011-02-08)
The Laranjeiras Gold Deposit (~1 Moz @6.32 g/t Au) is located at the eastern border of the Iron Quadrangle-QF, and is part of the Córrego do Sítio Lineament. It is hosted in intercalated Neo Archean, strongly foliated ...