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Joanne M. Whittaker

Researcher at University of Tasmania

Publications -  88
Citations -  4473

Joanne M. Whittaker is an academic researcher from University of Tasmania. The author has contributed to research in topics: Plate tectonics & Seafloor spreading. The author has an hindex of 32, co-authored 83 publications receiving 3471 citations. Previous affiliations of Joanne M. Whittaker include University of Sydney & Victoria University of Wellington.

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Response to Comment on "Major Australian-Antarctic Plate Reorganization at Hawaiian-Emperor Bend Time"

TL;DR: This work states that although it disagrees with Tikku and Direen's interpretations, the associated controversies reflect an absence of agreed-upon geophysical criteria for distinguishing stretched continental from oceanic crust, and a lack of samples from nonvolcanic margins.
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Australian-Antarctic breakup and seafloor spreading: Balancing geological and geophysical constraints

TL;DR: In this article, the most viable plate tectonic reconstructions were identified both with and without the input of the oldest, more controversial magnetic anomaly interpretations, and discussed implications for reconstructions of other margin pairs.
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The evolving paleobathymetry of the circum-Antarctic Southern Ocean since 34 Ma – A key to understanding past cryosphere-ocean developments

TL;DR: In this paper, the authors used more than 40 years of seismic reflection data acquisition along the margins of Antarctica and its conjugate margins, along with multiple drilling campaigns by the International Ocean Discovery Program (IODP) and its predecessor programs to calculate oceanwide paleobathymetry grids via a backstripping method.
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Mantle plumes and their role in Earth processes

TL;DR: The existence of mantle plumes was first proposed in the 1970s to explain intra-plate, hotspot volcanism, yet owing to difficulties in resolving mantle upwellings with geophysical images and discrepancies in interpretations of geochemical and geochronological data, the origin, dynamics and composition of plumes and their links to plate tectonics are still contested.
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Eastern Indian Ocean microcontinent formation driven by plate motion changes

TL;DR: In this article, a combination of plate tectonic reorganisation and plume-driven thermal weakening were required to calve the Batavia and Gulden Draak microcontinents in the Cretaceous Indian Ocean.