Peter Cawood

Professor

MONASH UNIVERSITY

Australia

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Peter Cawood is a Professor at Monash University in Australia. His research primarily focuses on geological processes, including paleoproterozoic metamorphism, mantle plume dynamics, and subduction zone geochemistry. Recent articles highlight his studies on the links between continental crust origins, volcanic CO2 emissions, and their implications for climate change. He is known for his contributions to understanding ancient crustal records and mass extinction events.

Peter Cawood

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Articles (28)

Paleoproterozoic metamorphic basement in Central Borneo: linking Indochina and Laurentia in Columbia

A two-stage mantle plume-sagduction origin of Archean continental crust revealed by water and oxygen isotopes of TTGs

Tin isotope systematics in subduction zones

Volcanic CO2 emissions from subduction of the tropical Paleo-Tethyan Ocean contributed to the early Permian deglacial warming

A geochemical and isotopic outline on the Alto Moxotó Terrane: a record of the best-preserved Paleoproterozoic crust in the central Borborema province, NE Brazil

Photic-zone euxinia had a major role in the Devonian-Carboniferous boundary mass extinction

Non-arc setting for “Cadomian” magmatism in Iran and Anatolia

Quantifying Magma Water Contents: A New Entrainment Model for Charnockite Formation

Zircon Inheritance Refines the Cambrian Orogenic Architecture of Southeast Australia

Lower crustal hot zones as zircon incubators: Inherited zircon antecryts in diorites from a mafic mush reservoir

Speculations on the Paleozoic legacy of Gondwana amalgamation

Syn-emplacement ophiolites and relationship to supercontinent cycle

On the Age-Old Problem of Dating a Granite: Combined Zircon, Apatite, and Titanite Petrochronology in an I-Type Granite from Mt Stirling, Australia

Low δ18O and δ30Si TTG at ca. 2.3 Ga Hints at an Intraplate Rifting Onset of the Paleoproterozoic Supercontinent Cycle

Cretaceous Coastal Mountain Building and Potential Impacts on Climate Change in East Asia

An amphibolitic source for “adakitic” I-type plutons in continental collision zones

A record of Neoarchaean cratonisation from the Storø Supracrustal Belt, West Greenland

Structural and geochronological constraints on the Portalegre shear zone: Implications for emerald mineralization in the Borborema Province, Brazil

Intraplate lithospheric extension revealed by seismic reflection profiling of South China

Paleogeographic Reconstruction of Precambrian Terranes Reworked by Phanerozoic Orogens: An Example Based on Detrital Zircon REE From Lhasa Terrane in Southern Tibet

I-type and S-type granites in the Earth’s earliest continental crust

The stability of cratons is controlled by lithospheric thickness, as evidenced by Rb-Sr overprint ages in granitoids

Enhanced Denudation of the Emeishan Large Igneous Province and Precipitation Forcing in the Late Permian

The stability of cratons is controlled by lithospheric thickness, as evidenced by Rb-Sr overprint ages in granitoids

An amphibolitic source for "adakitic" I-type plutons in continental collision zones

Secular Evolution of Continents and the Earth System

A resource for automated search and collation of geochemical datasets from journal supplements

Interplay between oceanic subduction and continental collision in building continental crust

Collaborators (14)

Jacob Mulder

Fabio Capitanio

Kristoffer Szilas

Erin Martin

roberto weinberg

Oliver Nebel

Edward Matheson

Laura Miller

Christopher Spencer

Stephen Johnston

Philip Heron

Sebastien Meffre

Peir Pufahl

Marc-Alban Millet

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