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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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Major Australian-Antarctic Plate Reorganization at Hawaiian-Emperor Bend Time

TL;DR: In this paper, a marked bend in the Hawaiian-Emperor seamount chain supposedly resulted from a recent major reorganization of the plate-mantle system there 50 million years ago.
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The breakup of East Gondwana: Assimilating constraints from Cretaceous ocean basins around India into a best‐fit tectonic model

TL;DR: In this paper, the authors link East Gondwana spreading corridors by integrating magnetic and gravity anomaly data from the Enderby Basin off East Antarctica within a regional plate kinematic framework to identify a conjugate series of east-west-trending magnetic anomalies, M4 to M0.
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GlobSed: Updated total sediment thickness in the World’s oceans

TL;DR: In this article, a new global 5 arc-minute total sediment thickness grid for the world's oceans and marginal seas is presented, GlobSed, which provides a much needed update of the sediment thickness distribution of the world oceans and delivers a model for sedimentation rates on oceanic crust through time that agrees well with selected drill data used for comparison.

Supporting Online Material for Major Australian-Antarctic Plate Reorganization at Hawaiian-Emperor Bend Time

TL;DR: In this article, a marked bend in the Hawaiian-Emperor seamount chain supposedly resulted from a recent major reorganization of the plate-mantle system there 50 million years ago.
Journal ArticleDOI

Constraining the Jurassic extent of Greater India: Tectonic evolution of the West Australian margin

TL;DR: In this paper, the authors present a new model that is constrained by revised seafloor spreading anomalies, fracture zones and crustal ages based on drillsites/dredges from all the abyssal plains along the West Australian margin and the Wharton Basin.