Richard Spikings

ORCID: 0000-0001-8949-8228
Publications
Citations
Views
---
Saved
---
About
Contact & Profiles
Research Areas
  • Geological and Geochemical Analysis
  • earthquake and tectonic studies
  • Geochemistry and Geologic Mapping
  • Geological and Tectonic Studies in Latin America
  • Geology and Paleoclimatology Research
  • High-pressure geophysics and materials
  • Geological Studies and Exploration
  • Paleontology and Stratigraphy of Fossils
  • Geological and Geophysical Studies
  • Hydrocarbon exploration and reservoir analysis
  • Geological Formations and Processes Exploration
  • Geological formations and processes
  • Geochemistry and Elemental Analysis
  • Mineralogy and Gemology Studies
  • Pleistocene-Era Hominins and Archaeology
  • Archaeology and ancient environmental studies
  • Geological and Geophysical Studies Worldwide
  • Isotope Analysis in Ecology
  • Landslides and related hazards
  • Radiation Detection and Scintillator Technologies
  • Groundwater and Isotope Geochemistry
  • Particle Detector Development and Performance
  • Heavy metals in environment
  • Botany and Geology in Latin America and Caribbean
  • Ancient Mediterranean Archaeology and History

University of Geneva
2015-2024

KU Leuven
2019

ETH Zurich
2001-2002

La Trobe University
1997-2001

Determining the absolute duration of magmatic-hydrothermal events leading to formation porphyry systems (i.e., including copper, skarn, and epithermal deposits) is one key questions in ore geology. This so because instrumental development genetic models necessary explore a category mineral deposits that provide most copper significant amounts base precious metals our economy. The problem determining has been addressed through thermal modeling cooling intrusions time needed precipitate...

10.2113/econgeo.108.4.565 article EN Economic Geology 2013-05-02

Research Article| June 01, 2015 Geochronology and Thermochronology Using Apatite: Time Temperature, Lower Crust to Surface David M. Chew; Chew 1Department of Geology, School Natural Sciences, Trinity College DublinDublin 2, IrelandE-mail: chewd@tcd.ie Search for other works by this author on: GSW Google Scholar Richard A. Spikings 2Section Earth Environmental University GenevaCH-1205, Geneva, SwitzerlandE-mail: Richard.Spikings@unige.ch Author Article Information Publisher: Mineralogical...

10.2113/gselements.11.3.189 article EN Elements 2015-06-01

We investigated the Neoproterozoic–early Paleozoic evolution of Gondwanan margin north-central Andes by employing U-Pb zircon geochronology in Eastern Cordilleras Peru and Ecuador using a combination laser-ablation–inductively coupled plasma–mass spectrometry detrital analysis dating syn- post-tectonic intrusive rocks thermal ionization mass ion microprobe. The majority samples exhibits prominent peaks ranges 0.45–0.65 Ga 0.9–1.3 Ga, with minimal older detritus from Amazonian craton. These...

10.1130/b26080.1 article EN Geological Society of America Bulletin 2007-03-21

Research Article| September 01, 2009 Tectonomagmatic evolution of Western Amazonia: Geochemical characterization and zircon U-Pb geochronologic constraints from the Peruvian Eastern Cordilleran granitoids Aleksandar Mišković; Mišković † 1Department Mineralogy, Earth Sciences Section, University Geneva, 13 rue des Maraîchers, CH-1205 Switzerland *Current address: Earth, Atmospheric, Planetary Sciences, Massachusetts Institute Technology, 77 Avenue (54-1224), Cambridge, 02139, USA. †E-mail:...

10.1130/b26488.1 article EN Geological Society of America Bulletin 2009-07-21

Abstract The determination of accurate and precise ages for the timing collision between oceanic plateaus continental crust requires an understanding how indenting buttressing plates respond to collision. We present geochronological, thermochronological, geochemical isotopic analyses magmatic rocks from Ecuadorian Andes, which relate Late Cretaceous Caribbean Plateau Great Arc sequence with NW South America. cessation subduction magmatism during 65–64 Ma beneath eastern edge was synchronous...

10.1111/j.1365-3121.2006.00688.x article EN Terra Nova 2006-06-21

The topographically prominent Sierra Nevada de Santa Marta forms part of a faulted block continental crust located along the northern boundary South American Plate, hosts highest elevation in world (∼5.75 km) whose local base is at sea level, and juxtaposes oceanic plateau rocks Caribbean Plate. Quantification amount timing exhumation constrains interpretations history plate boundary, driving forces rock uplift active margin. Province southernmost exhumed elevated rates (≥0.2 Km/My) during...

10.1029/2010tc002835 article EN public-domain Tectonics 2011-07-21
Coming Soon ...