Galen P. Halverson focuses on Paleontology, Glacial period, Snowball Earth, Marinoan glaciation and Cap carbonate. In his study, which falls under the umbrella issue of Paleontology, Geologic record is strongly linked to Chemostratigraphy. His Glacial period study combines topics from a wide range of disciplines, such as Precambrian and Sea level.
His studies deal with areas such as Sedimentary basin, Earth science, Rodinia, Supercontinent and Tonian as well as Snowball Earth. Galen P. Halverson focuses mostly in the field of Marinoan glaciation, narrowing it down to topics relating to Continental shelf and, in certain cases, Thermal subsidence, Waves and shallow water, Unconformity, Dolomite and Deep sea. His biological study spans a wide range of topics, including Dolostone and Diamictite.
Galen P. Halverson mainly focuses on Paleontology, Geochemistry, Glacial period, Snowball Earth and Proterozoic. His research related to Sedimentary rock, Diamictite, Cap carbonate, Marinoan glaciation and Dolostone might be considered part of Paleontology. His Geochemistry study incorporates themes from Rodinia and Chemostratigraphy, Isotopes of carbon.
His work carried out in the field of Glacial period brings together such families of science as Stratotype, Period, Tonian and Supercontinent. The concepts of his Snowball Earth study are interwoven with issues in Meltwater, Continental shelf, Earth science and Weathering. His Proterozoic research is multidisciplinary, incorporating elements of Anoxic waters, Geochronology, Seawater, Precambrian and Geologic time scale.
His primary areas of study are Geochemistry, Proterozoic, Paleontology, Tonian and Sedimentary rock. His research in Geochemistry intersects with topics in Sedimentary depositional environment and Chemostratigraphy, Isotopes of carbon. His Proterozoic research incorporates themes from Geologic time scale, Earth science, Arctic and Archean.
His studies in Geochronology, Glacial period, Snowball Earth, Laurentia and Structural basin are all subfields of Paleontology research. His Glacial period study combines topics in areas such as Period and Stratotype. He has researched Snowball Earth in several fields, including Meltwater and Marinoan glaciation.
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A Neoproterozoic Snowball Earth
Paul F. Hoffman;Alan J. Kaufman;Galen P. Halverson;Daniel P. Schrag.
Toward a Neoproterozoic composite carbon-isotope record
Galen P. Halverson;Paul F. Hoffman;Daniel P. Schrag;Adam C. Maloof.
Geological Society of America Bulletin (2005)
Evolution of the 87Sr/86Sr composition of Neoproterozoic seawater
Galen P. Halverson;Francis Ö. Dudás;Adam C. Maloof;Samuel A. Bowring.
Palaeogeography, Palaeoclimatology, Palaeoecology (2007)
On the initiation of a snowball Earth
Daniel P. Schrag;Robert A. Berner;Paul F. Hoffman;Galen P. Halverson.
Geochemistry Geophysics Geosystems (2002)
Statistical analysis of iron geochemical data suggests limited late Proterozoic oxygenation
Erik Sperling;Erik Sperling;Erik Sperling;Charles J. Wolock;Alex S. Morgan;Benjamin C. Gill.
Neoproterozoic glaciations in a revised global palaeogeography from the breakup of Rodinia to the assembly of Gondwanaland
Zheng-Xiang Li;Zheng-Xiang Li;David A.D. Evans;Galen P. Halverson;Galen P. Halverson.
Sedimentary Geology (2013)
Are basal Ediacaran (635 Ma) post-glacial “cap dolostones” diachronous?
Paul F. Hoffman;Galen P. Halverson;Eugene W. Domack;Jonathan M. Husson.
Earth and Planetary Science Letters (2007)
Comings and Goings of Global Glaciations on a Neoproterozoic Tropical Platform in Namibia
Paul F. Hoffman;Alan J. Kaufman;Galen P. Halverson.
Snowball Earth climate dynamics and Cryogenian geology-geobiology
Paul F. Hoffman;Paul F. Hoffman;Dorian S. Abbot;Yosef Ashkenazy;Douglas I. Benn.
Science Advances (2017)
A major perturbation of the carbon cycle before the Ghaub glaciation (Neoproterozoic) in Namibia: Prelude to snowball Earth?
Galen P. Halverson;Paul F. Hoffman;Daniel P. Schrag;Alan J. Kaufman.
Geochemistry Geophysics Geosystems (2002)
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