People
Daniel Moncada is an Assistant professor in the Department of Geology, University of Chile. Daniel´s teaching and research experience includes the role of fluids in planetary processes and the physical and geochemical environment of formation of mineral deposits. Daniel has been working in Mexico, Turkey, USA, Chile, Argentina, and China combining numerical modeling, geochemistry, structural geology, mapping surface and underground mines, logging drill core, resource modeling and estimation, remote sensing, assistance in planning exploration projects. Daniel's interests include playing (running and racketball)
Claudia Cannatelli´s research is focused on the understanding of how the Earth´s internal processes contribute to producing magmatism and volcanism. She investigates the roles that volatiles play in melting, crystallization, degassing, style and frequency of volcanic eruptions by combining melt inclusions studies and thermodynamic modeling. She is also interested in mantle melting processes and magma genesis in subduction zones. Dr. Cannatelli teaches courses in Physical Volcanology, Fluids in Planetary Systems and Environmental Geochemistry. As associate researcher at Andean Geothermal Center of Excellence (CEGA), she works in the “Heat Sources” and “Fluid Geochemistry” research groups, at the University of Chile.
Jamie studies the impact of tectonics and climate on the landscape development of mountain belts. He utilizes low-temperature thermochronometry and ArcGIS DEM analyses to quantify the long-term exhumation and recent surface response generated by tectonic uplift and/or climatic forcing of orogens at active plate margins. He applies (U-Th)/He and fission track dating to bedrock samples to help identify the areal extent of thermal anomalies and time stamp when rocks were heated above closure temperature in geothermally active regions in the Patagonia.
David Calisto is a geologist from University of Chile. David´s MS research is focused on understanding the processes of mineral precipitation in active and fossil geothermal systems in Chile.
Martin Cerda is an undergraduate student at University of Chile, working on his senior thesis.
Agustin Valenzuela is an undergraduate student at University of Chile, working on his senior thesis.
Jorge Ibanez is an undergraduate student at University of Chile, working on his senior thesis.
Christopher Yáñez is an undergraduate student at University of Chile, working on his senior thesis.
María Eugenia Parra is an undergraduate student at University of Chile, working on her senior thesis.
Nicolas Ayala is an undergraduate student at University of Chile, working on his senior thesis.
Daniel Austillo is an undergraduate student at University of Chile, working on his senior thesis.
Loreto Hernández is a geologist from University of Chile, who is working on her PhD.
Franco Robbiano is an undergraduate student at University of Chile, working on his senior thesis.
Fabián Tapia is an undergraduate student at University of Chile, working on his senior thesis.
Samanta Aravena is a geologist from University of Chile, working on her MS.
Nicolas Avalos is an undergraduate student at University of Chile, working on his MS.
Former Students
Cristóbal Aracena is graduate student at University of Chile
Alicia Zúñiga is graduate student at University of Chile, working on her senior thesis. Her research is focused on the acid salt pan in the Northern part of Chile, by looking at fluid inclusions and microorganism into sulfate and halite minerals. Now she is working in solving problems in the hydroworld.
Bastián Muñoz is an undergraduate student at University of Chile, working on his senior thesis. His research is aimed to understand the evolution of fluids in the Chancón Mining District, with the main goal of estimate its potential as energy resource, and is study is focused on the analysis of fluid inclusions in opaque minerals by using an infrared camera.
Aracely Ramírez is an undergraduate student at University of Chile, working on her senior thesis. Aracely works in the acid salt pans in the Northern part of Chile, by looking at fluid inclusions and microorganism into sulfate minerals.
Juan Pablo Tapia is an undergraduate student at University of Chile, working on his senior thesis. His research is focused in the estimation of REEs concentrations into the fluid from pegmatites minerals, with applications in energy-related technologies.
Juan Ignacio is an undergraduate student from University of Chile, working on his senior thesis. He is working on the epithermal system at Cerro Bayo, Aysén to understand the distribution of boiling events and mineralization.
Andrés Gómez is a geologist from University of Chile. For his senior thesis, Andrés focused his study on the petrology of the Southernmost part of Chile, the Magallanes and Chilean Antarctica. He has also worked in the application of geochemistry, surface mapping and study of drill cores for epithermal gold deposits exploration in the northern Andes of Chile. He is currently a Master Student and his research is focused on the understanding of the Alhué mining district through the study of the mineralizing fluids, which are thought to be responsible of mineralized veins with Au-Ag contents. As a hobby, he is very passionate about all nautical sports. Bernardita Alvear is a geologist from University of Chile. Bernardita´s research is focused on understanding the processes of mineral precipitation in active geothermal systems, such as Puchuldiza, Tolhuaca and Cerro Pabellón. She is looking at the different types of silica precipitation, textures and crystallization. She uses different analytical techniques, including SEM, LA-ICP-MS, XRD and FTIR. Bernardita is a Master student of the Andean Geothermal Centre of Excellence (CEGA). She likes riding a bike and doing crafts. Mariana Wong is an undergraduate student at University of Chile, who is working on her senior thesis.
Nicolas Amengual is an undergraduate student at University of Chile, who is working on his senior thesis.
Fluids Research Lab at Virginia Tech
We are currently seeking MSc and PhD students for starting in the Fall semester of 2020. Interested students, please contact Daniel Moncada or Claudia Cannatelli directly,to discuss research projects and opportunities
Collaborators, friends and Research Links
Research
The pegmatites display aspects of both igneous and hydrothermal systems and have fascinated the geologist for the barren exotic minerals and inclusionist for the daughter minerals. In more recently years the “Great Element Hunt” have been mined on a small scale around the world. This research focuses on granite and pegmatite located in Aysén region, looking the REEs minerals and the technological applications.
The evolution of the epithermal mineralization can be modeled if know the mineral speciation, mechanism of precipitation, volatiles dissolved in the aqueous phase using the software TOUGHREACT. This software can simulate the multiphase fluid flow (i.e., water, water vapor, CO2) and aqueous and gaseous species transport in fractured media that drives the formation of vein-filling
Hot waters rise convectively in geothermal systems, they interact with the host rock removing some components such as silica and the interaction water rock creates mew mineral suite. Silica and carbonate phases in the geothermal systems often show highly variable and sometimes diagnostic textures. In this research we are looking growth zone of silica and carbonate phases using cathodoluminescence, and other analytical techniques. The result shows the complexity of these phases with deformation, dissolution, and healing are especially difficult to establish using standard techniques (e.g. petrographic microscope).
The alteration in active geothermal areas into Maipo Valley is one of the least understood aspects. The gold of this study in characterized in time and space the distribution of the different alteration presents in that area.
Geothermal fluids contain dissolved solids under conditions of elevated temperatures and pressure. The most common components present in geothermal systems are silica, calcium carbonate in some cases precious and base metals. In geothermal systems in the Andes there is little work related to geothermal fluids and associated mineral and their use for strategic mineral exploration. In our research, we focus on two active hydrothermal systems,the Irruputuncu and Olca volcanoes which are located between Chile and Bolivia
Assessment of the geologic and geodynamic setting including the structural analysis focused primarily on geothermal targets Those features might be recorded on hydrothermal fluids in faults, fractures and folds because fluid pathways are critical for the productivity of reservoir and are commonly controlled by structuress.
EXPLORATION FOR MINERAL DEPOSITS
Exploration for mineral deposits is an expensive and high-risk venture. Organizations that can evaluate prospects more quickly and inexpensively than its competitors and discriminate between prospects with high and low potential for economic mineralization will thus have a significant competitive advantage. Empirical models (that may or not be based on genetic models) are what drive successful exploration programs, and the successful explorationist is one who is able to recognize critical components of these models in outcrop and drill core samples.
Recognizing the need for rapidfield-based analysis in orogenic gold deposits, in this study we are developing and building a portable fluid-inclusion crushing stage using a 3D printer. The crushing stage will be used to study the fluid inclusions in different host minerals (e.g. quartz, feldspar) in the exploration for Au-rich vein deposits in the metamorphic basement in Chile, especially in areas with limited or non-existent outcrop.
Alhué mining district is located southwest of Santiago city within the Coastal Range of Central Chile and 24 kilometers east of the locality of Villa Alhué, and is characterize by numerous Au-Ag veins (more than 76) of hydrothermal origin with different thicknesses related to major and minor, normal and strike-slip faults with significant displacement and trending N25ºW trending
Fluids from Chancón mining district located southwest of Santiago within the Coastal Range of Central Chile shows gold and base metal that in recent years a wide variety of “Rare Earth Metals”, including selenium, indium and tellurium, have found important applications in energy-related technologies such as advanced photovoltaic solar cells. These metals are produced commercially as a byproduct in the refining of porphyry copper and similar ores, and from selenium and tellurium-rich epithermal deposits.
Numerous studies have documented the close association between boiling and mineralization in the epithermal environment. Located in the Chilean Patagonia, Cerro Bayo, Aysén preserves a low-sulfidation epithermal deposit showing different boiling events. Boiling Textural evidence of colloform-silica texture and bladed calcite replaced by quartz has been documented and the spatial distribution can provided vector toward to exploration.
FLUID INCLUSIONS IN SEDIMENTARY AND DIAGENETIC SYSTEMS
Acid salars in the northern part of Chile creates an environment to study the evolution of microorganism trapped as a single homogeneous fluid into sulfate and halite minerals. Combining petrography of fluid inclusions assemblages (FIA), chemical and biological non-destructives methods might provide the time-lapse of growth crystals and type of microorganism.
Collaborators, friends and Research Links
Fluids Research Lab at Virginia Tech
Publications
Book Chapters:
Published/in press articles:
Honor Thesis
Patent
Press
Facilities
Analog IR camera to 2200nm with computer interface, Digital color camera with IR monochrome capabilities to 1000nm
Linkam THMSG600 heating-cooling stage complete with digital software package
Linkam TS 1400XY high temperature stage with digital software package
USGS cooling/heating stage
Lab-RAM
High spatial and spectral resolutions
Allowing the determination of crystallinity, polymorphism, strain and other band analysis.
From UV to NIR
AAllowing detailed sample characterization from many varied materials.
Ultra-fast confocal imaging
DuoScan™ - high precision, ultra-fast rastering mirrors creating variable sized laser macro-spots, allowing nano-step mapping.
Ultra-Low Frequency Module
Allows additional sample characterization to be made in a spectral region rarely available with other basic spectrometers.
High spatial and spectral resolutions
Allowing the determination of crystallinity, polymorphism, strain and other band analysis.
From UV to NIR
AAllowing detailed sample characterization from many varied materials.
Ultra-fast confocal imaging
DuoScan™ - high precision, ultra-fast rastering mirrors creating variable sized laser macro-spots, allowing nano-step mapping.
Ultra-Low Frequency Module
Allows additional sample characterization to be made in a spectral region rarely available with other basic spectrometers.
Allowing the determination of crystallinity, polymorphism, strain and other band analysis.
From UV to NIR
AAllowing detailed sample characterization from many varied materials.
Ultra-fast confocal imaging
DuoScan™ - high precision, ultra-fast rastering mirrors creating variable sized laser macro-spots, allowing nano-step mapping.
Ultra-Low Frequency Module
Allows additional sample characterization to be made in a spectral region rarely available with other basic spectrometers.
From UV to NIR
AAllowing detailed sample characterization from many varied materials.
Ultra-fast confocal imaging
DuoScan™ - high precision, ultra-fast rastering mirrors creating variable sized laser macro-spots, allowing nano-step mapping.
Ultra-Low Frequency Module
Allows additional sample characterization to be made in a spectral region rarely available with other basic spectrometers.
AAllowing detailed sample characterization from many varied materials.
Ultra-fast confocal imaging
DuoScan™ - high precision, ultra-fast rastering mirrors creating variable sized laser macro-spots, allowing nano-step mapping.
Ultra-Low Frequency Module
Allows additional sample characterization to be made in a spectral region rarely available with other basic spectrometers.
Ultra-fast confocal imaging
DuoScan™ - high precision, ultra-fast rastering mirrors creating variable sized laser macro-spots, allowing nano-step mapping.
Ultra-Low Frequency Module
Allows additional sample characterization to be made in a spectral region rarely available with other basic spectrometers.
DuoScan™ - high precision, ultra-fast rastering mirrors creating variable sized laser macro-spots, allowing nano-step mapping.
Ultra-Low Frequency Module
Allows additional sample characterization to be made in a spectral region rarely available with other basic spectrometers.
Ultra-Low Frequency Module
Allows additional sample characterization to be made in a spectral region rarely available with other basic spectrometers.
Allows additional sample characterization to be made in a spectral region rarely available with other basic spectrometers.
- Sample preparation: “quick plates” and polished sections, and mineral mounts
- Scanning electron microscope (SEM) with SE, BSE, EDS and CL detectors. The laboratory will be equipped with carbon/gold coaters, sample preparation area and image processing/data manipulation
- Geochemistry Laboratory: atomic absorption spectrometry (AAS), ion chromatography (IC), optical emission inductively coupled plasma spectrometer (ICP-OES), and LA-ICP-MS (Thermo Fisher Science Quadrupole attached to a Photon Machinnes Analyte G2 ArF Excimer Laser Ablation system)
- Isotope Geochemistry Laboratory: laser-ablation multiple-collector inductively coupled plasma mass spectrometry system, LA-MC-ICP-MS (Thermo Neptune Plus, with a 193 nm Ar-F Photon Machines Laser Ablation system)
Contact
Address
Facultad de Cs. Fís. y Matem.
Universidad de Chile
Plaza Ercilla 803, Santiago, Chile
Telephone:
+56-2-29784116 Claudia Cannatelli
+56-2-29784118 Daniel Moncada
Fax: +56-2-26963050