Fellow of the Geological Society of America
Joseph G. Meert mainly investigates Paleontology, Supercontinent, Rodinia, Gondwana and Craton. His Paleontology study focuses mostly on Paleomagnetism, Baltica, Apparent polar wander, Paleozoic and Tectonics. His study in Paleomagnetism is interdisciplinary in nature, drawing from both Earth science and Geochronology.
His Supercontinent study frequently draws connections to adjacent fields such as Laurentia. Joseph G. Meert has included themes like Precambrian, Mafic, Proterozoic and Zircon in his Rodinia study. His study explores the link between Gondwana and topics such as Orogeny that cross with problems in Mozambique Belt and Terrane.
Joseph G. Meert focuses on Paleontology, Paleomagnetism, Geochemistry, Gondwana and Craton. Supercontinent, Rodinia, Laurentia, Baltica and Proterozoic are among the areas of Paleontology where Joseph G. Meert concentrates his study. His biological study spans a wide range of topics, including Paleozoic, Precambrian, Tectonics and Geochronology.
As part of one scientific family, Joseph G. Meert deals mainly with the area of Geochemistry, narrowing it down to issues related to the Magmatism, and often Igneous rock. His work deals with themes such as Orogeny, Shear zone, Earth science and Mozambique Belt, which intersect with Gondwana. In his work, Polar wander and Aridification is strongly intertwined with True polar wander, which is a subfield of Apparent polar wander.
Joseph G. Meert mainly focuses on Geochemistry, Paleontology, Craton, Paleomagnetism and Archean. His research integrates issues of Magmatism and Terrane in his study of Geochemistry. His work on Supercontinent, True polar wander and Rodinia as part of general Paleontology research is frequently linked to East Asia, thereby connecting diverse disciplines of science.
His Supercontinent research includes elements of Geochronology, Proterozoic and Tectonic zone. His Apparent polar wander study in the realm of Paleomagnetism connects with subjects such as Intersection. The various areas that he examines in his Zircon study include Orogeny and Gondwana.
His scientific interests lie mostly in Geochemistry, Paleontology, Paleomagnetism, Large igneous province and Craton. His Geochemistry study which covers Terrane that intersects with Subduction and Lithosphere. His Paleontology study frequently links to other fields, such as Aridification.
His work carried out in the field of Paleomagnetism brings together such families of science as Permian, Tectonics and Plate reconstruction. His studies in Craton integrate themes in fields like Hadean, Mantle and Crust. Joseph G. Meert combines subjects such as Dharwar Craton, Granulite, Gondwana and Zircon with his study of Archean.
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A synopsis of events related to the assembly of eastern Gondwana
Joseph G Meert.
Tectonophysics (2003)
Continental break-up and collision in the Neoproterozoic and Palaeozoic — A tale of Baltica and Laurentia
T.H. Torsvik;M.A. Smethurst;J.G. Meert;R. Van der Voo.
Earth-Science Reviews (1996)
Phanerozoic polar wander, palaeogeography and dynamics
Trond H. Torsvik;Rob Van der Voo;Rob Van der Voo;Ulla Preeden;Conall Mac Niocaill.
Earth-Science Reviews (2012)
Paleomagnetic constraints on timing of the Neoproterozoic breakup of Rodinia and the Cambrian formation of Gondwana
C.Mca. Powell;Zheng-Xiang Li;M.W. Mcelhinny;J.G. Meert.
Geology (1993)
The making and unmaking of a supercontinent: Rodinia revisited
Joseph G. Meert;Trond H. Torsvik.
Tectonophysics (2003)
The Neoproterozoic assembly of Gondwana and its relationship to the Ediacaran–Cambrian radiation
Joseph G. Meert;Bruce S. Lieberman.
Gondwana Research (2008)
THE PROTEROZOIC SUPERCONTINENT RODINIA : PALEOMAGNETICALLY DERIVED RECONSTRUCTIONS FOR 1100 TO 800 MA
Arlo B Weil;Rob Van der Voo;Conall Mac Niocaill;Joseph G Meert.
Earth and Planetary Science Letters (1998)
Palaeomagnetic configuration of continents during the Proterozoic
L.J. Pesonen;S.-Å. Elming;S. Mertanen;S. Pisarevsky.
Tectonophysics (2003)
What's in a name? The Columbia (Paleopangaea/Nuna) supercontinent
Joseph G. Meert.
Gondwana Research (2012)
A ‘snowball Earth’ climate triggered by continental break-up through changes in runoff
Yannick Donnadieu;Yves Goddéris;Gilles Ramstein;Anne Nédélec.
Nature (2004)
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