Diverse subaerial and sublacustrine hot spring settings of the Cerro Negro epithermal system (Jurassic, Deseado Massif), Patagonia, Argentina

2012 ◽  
Vol 229-230 ◽  
pp. 1-12 ◽  
Author(s):  
Diego M. Guido ◽  
Kathleen A. Campbell
Ameghiniana ◽  
2016 ◽  
Vol 53 (2) ◽  
pp. 205-230 ◽  
Author(s):  
Juan García Massini ◽  
Ignacio H. Escapa ◽  
Diego M. Guido ◽  
Alan Channing
Keyword(s):  

2016 ◽  
Vol 51 (6) ◽  
pp. 725-748 ◽  
Author(s):  
Conrado Permuy Vidal ◽  
Diego M. Guido ◽  
Sebastián M. Jovic ◽  
Robert J. Bodnar ◽  
Daniel Moncada ◽  
...  

SEG Discovery ◽  
2011 ◽  
pp. 1-23
Author(s):  
D. SHATWELL ◽  
J. A. CLIFFORD ◽  
D. ECHAVARRÍA ◽  
G. IRUSTA ◽  
D. LOPEZ

ABSTRACT Exploration by Andean Resources Ltd. in the Cerro Negro district of southern Argentina between March 2005 and July 2010 delineated resources of 2.54 Moz gold and 23.5 Moz silver in three low-sulfidation epithermal vein deposits. Two of these, Eureka West and Bajo Negro, are new discoveries; the third deposit, Vein Zone, had been explored previously. Additional measured and indicated resources of 2.7 Moz Au have been estimated by current owners Goldcorp Inc. for three other discoveries at Cerro Negro: San Marcos, Mariana Norte, and Mariana Central. The total gold resource for the project is 5.3 Moz Au measured and indicated, plus 1.24 Moz inferred. Andean completed a positive feasibility study into an underground and open pit mining operation in July 2010, based on reserves of 2.07 Moz Au and 20.6 Moz Ag at Eureka, Bajo Negro, and Vein Zone. The study concluded that these deposits can produce an average of 200,000 oz of gold and 1.8 Moz of silver per year for 10 years, which would make Cerro Negro the largest gold producer in the Deseado Massif without considering resources or production from the other three deposits. The deposits are hosted by Late Jurassic volcanic and probable intrusive rocks of the Deseado Massif in which Triassic-Cretaceous extension created the structures which control the precious metal vein deposits. Four of the five new discoveries were found through geologic mapping, but pioneering work by previous explorers also contributed; the two most recent discoveries do not crop out. Geophysical studies helped to define drill targets and are likely to be increasingly important in future exploration. A key ingredient in Andean’s success was a willingness to drill test targets identified by a skilled and dedicated, largely Argentine, exploration team, supported by Australian and North American-based management.


2007 ◽  
Vol 144 (2) ◽  
pp. 401-411 ◽  
Author(s):  
ALAN CHANNING ◽  
ALBA B. ZAMUNER ◽  
ADOLFO ZÚÑIGA

We present an initial report of a well-preserved and relatively diverse Gondwanan plant assemblage from Bahía Laura Group, Chon Aike Formation strata of the Estancia Flecha Negra area, central-western region of the Deseado Massif, Santa Cruz province, Patagonia, Argentina. The locality contains the first richly fossiliferous chert with a diverse and well-preserved plant assemblage reported from the Mesozoic which is demonstrably associated with hot spring activity. A compression flora and petrified forest contained in associated clastic and volcaniclastic environments provide an indication of regional plant diversity during this as yet poorly represented stratigraphic interval.


2019 ◽  
Vol 156 (9) ◽  
pp. 1631-1638 ◽  
Author(s):  
Diego M Guido ◽  
Kathleen A Campbell ◽  
Frédéric Foucher ◽  
Frances Westall

AbstractJurassic siliceous hot-spring (sinter) deposits from Argentine Patagonia were evaluated to determine the distribution and preservation quality of their entombed microbial fabrics. Detailed study showed that the Claudia palaeo-geothermal field hosts the best-preserved sinter apron in the Deseado Massif geological province, where we also found hot-spring silica–biotic interactions extending into hydrothermally influenced fluvial and lacustrine settings. Carbonaceous material was identified by petrography and Raman spectroscopy mapping; it is inter-laminated with silica across proximal vent to distal marsh facies. The ubiquitous presence of microbial biosignatures has application to studies of hydrothermal settings of early life on Earth and potentially Mars.


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