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Mohammad Ayaz Alam

Departamento de Geología
Universidad de Chile
Plaza Ercilla 803, Santiago
Chile
Tel: (56 2) 9780725
Fax: (56 2) 6963050
ayaz@ing.uchile.cl
Postdoctoral Researcher (Project PBCT PDA-07)

Academic Qualifications
Doctor of Philosophy (Ph.D.), Indian Institute of Technology Bombay, Mumbai, India (2008)
Thesis: Geological, Geochemical and Geothermal Studies on the Barren Island Volcano, Andaman Sea, Indian Ocean
Master of Science (Applied Geology), Indian Institute of Technology Bombay, Mumbai, India (2002)
Dissertation: Hydrogeochemistry of Thermal Springs of Manikaran, Kullu District, Himachal Pradesh, India

Degree Awarded in Recognition
Doctor en Geología (Doctor in Geology), Universidad de Chile, Santiago, Chile (2010)

Professional Title
Título de Geólogo (Title of Geologist), Universidad de Chile, Santiago, Chile (2010)

Specialization
Geothermal Geochemistry, Hydrogeochemistry, Volcanology, Igneous Petrology

Current Research
Study of the nature, geochemistry and heat source of the geothermal manifestations along the Liquiñe-Ofqui Fault Zone (LOFZ) in the south-central volcanic zone of Chile (southern Chilean Andes), to understand the interplay of volcanism and structural control for the geothermal systems.

Focus Areas
Geothermal Investigations in Central and Southern Chilean Andes
Barren Island and Narcondam volcanoes (Andaman Sea, Indian Ocean)

Teaching
Geothermal Geochemistry (Geoquímica Geotérmica). Developed and introduced from the Autumn Semester of 2010.

Supervision of the Dissertations: (One completed, two in progress)

Languages: English, Spanish, Hindi, Marathi, Urdu

Journal articles

2010
2009
2004
M A Alam, D Chandrasekharam, O Vaselli, B Capaccioni, P Manetti, A P Santo (2004)  Petrology of the prehistoric lavas and dyke of the Barren Island, Andaman Sea, Indian Ocean   Journal of Earth System Science 113: 4. 715-721 December  
Abstract: Although Barren Island (Andaman Sea, Indian Ocean) witnessed several volcanic eruptions during historic times, the eruptions that led to the formation of this volcanic island occurred mainly during prehistoric times. It is still active and currently in the fumarolic stage. Its volcanic evolution appears to be characterized by a constructive phase with the piling up of lava flows and scoria deposits and Strombolian activities, followed by a sudden collapse of the main cone. Deposits of a possible caldera-forming eruption were not recognized earlier. After a period of peri-calderic hydromagmatic activity, whose deposits presently mantle inner and outer caldera walls, a new phase of intracalderic Vulcanian activities took place. A prominent dyke in the SE inner side of the caldera wall was recognized. Petrographically the lava flows and dyke are similar but they differ in their chemical composition (viz., SiO2, MgO, Ni, Cr) significantly. Similarity in major, minor and trace element composition (viz., K/La, K/Nb, K/Rb, K/Ti ratios) of these rocks together with Chondrite normalized trace element (Rb, Ba, Sr, P, Zr, Ti and Nb) and REE (La, Ce, Nd and Y) patterns of the Barren Island prehistoric lava flows and dyke and low-K lavas of Sunda Arc indicates that Barren Island must have evolved from a source similar to that of Sunda Arc lavas during the Quaternary Period.
Notes:
2003

Book chapters

2010
2004

Conference papers

2009
2005
2003
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