Zobrazeno 1 - 10
of 16
pro vyhledávání: '"Brian A. Konecke"'
Autor:
Santiago Tassara, Martin Reich, Brian A. Konecke, José María González-Jiménez, Adam C. Simon, Diego Morata, Fernando Barra, Adrian Fiege, Manuel E. Schilling, Alexandre Corgne
Publikováno v:
Frontiers in Earth Science, Vol 8 (2020)
The oxidation state of the Earth’s mantle and its partial melting products exert a key control on the behavior and distribution of sulfur and chalcophile and siderophile elements between the mantle and crust, underpinning models of ore deposit form
Externí odkaz:
https://doaj.org/article/4b01550bf5d04424ab0025ddbb59259a
Autor:
Jackie M. Kleinsasser, Adam C. Simon, Brian A. Konecke, Michael J. Kleinsasser, Philipp Beckmann, François Holtz
Publikováno v:
Geochimica et Cosmochimica Acta. 326:1-16
Autor:
Timm John, Esther M. Schwarzenbach, Santiago Tassara, Ji-Lei Li, Jay J. Ague, Jun Gao, Brian A. Konecke
Publikováno v:
Geochimica et Cosmochimica Acta. 297:40-64
Subduction zones mediate the sulfur exchange between Earth’s interior and surface, and play a critical role in the long-term global sulfur cycle. Dehydration of the subducted slab releases aqueous fluids, which in turn interact with the surrounding
Autor:
Mathieu Leisen, Martin Reich, Fernando Barra, Tristan M. Childress, J. Tomás Ovalle, Nikita L. La Cruz, Brian A. Konecke, Adam C. Simon
Publikováno v:
Economic Geology. 115:1461-1491
The textures of outcrop and near-surface exposures of the massive magnetite orebodies (>90 vol % magnetite) at the Plio-Pleistocene El Laco iron oxide-apatite (IOA) deposit in northern Chile are similar to basaltic lava flows and have compositions th
Autor:
Martin Reich, Fernando Barra, Santiago Tassara, Eduardo Morgado, Adam C. Simon, Brian A. Konecke, Mathieu Leisen, C. Cannatelli, Adrian Fiege, D. Kausel, Diego Morata
Publikováno v:
Geochimica et Cosmochimica Acta. 273:291-312
Iniciativa Cientifica Milenio, through grant "Millennium Nucleus for Metal Tracing along Subduction". Comision Nacional de Investigacion Cientifica y Tecnologica (CONICYT), CONICYT FONDAP: 15090013. CONICYT-FONDEQUIP grants: EQM120098, EQM140009. Com
Publikováno v:
Geochimica et Cosmochimica Acta. 265:242-258
The incorporation of sulfur (S) into the apatite structure and the partitioning of S between apatite and silicate melt (DSap/m) have been proposed to vary systematically as a function of prevailing redox conditions. In this study, we experimentally e
Publikováno v:
Ore Geology Reviews. 107:1084-1096
The oxidation state of sulfur (S) plays a critical role in the formation of igneous and hydrothermal mineral systems. Constraining the oxidation state of S during mineralization and alteration is a valuable tool for understanding primary versus secon
Publikováno v:
Goldschmidt2021 abstracts.
Publikováno v:
Geological Society of America Abstracts with Programs.
Autor:
J. Tomás Ovalle, Maria A. Rodriguez-Mustafa, Artur P. Deditius, Martin Reich, Adam C. Simon, Diego Morata, Tristan M. Childress, Fernando Barra, Brian A. Konecke, Nikita L. La Cruz
Publikováno v:
Scientific Reports, Vol 8, Iss 1, Pp 1-11 (2018)
Scientific Reports
Artículos CONICYT
CONICYT Chile
instacron:CONICYT
Scientific Reports
Artículos CONICYT
CONICYT Chile
instacron:CONICYT
The genetic link between magmas and ore deposit formation is well documented by studies of fossil hydrothermal systems associated with magmatic intrusions at depth. However, the role of explosive volcanic processes as active agents of mineralization