Dr Maria Seton

Maria SetonAcademic Staff

maria.seton@sydney.edu.au

Phone: +61 2 9351 4255
Fax: +61 2 9351 2442

Madsen Building F09, Room 400
School of Geosciences
The University of Sydney
Sydney, NSW 2006
Australia

View Maria's Sydney Uni page

See below for EarthByte content related to Maria.

Plate reconstructions of Southeast Asia

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This animation is from our recent work on Southeast Asian plate reconstructions.Read the peer-reviewed paperCitationZahirovic, S., M. Seton, and R. Müller (2014), The Cretaceous and Cenozoic tectonic evolution of Southeast Asia, Solid Earth (EGU), 5, 227-273. doi: 10.5194/se-5-227-2014.View similar animations on our EarthByte YouTube channel

Solid Earth – The Cretaceous and Cenozoic tectonic evolution of Southeast Asia

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Zahirovic, S., Seton, M., & Müller, R. D. (2014). The Cretaceous and Cenozoic tectonic evolution of Southeast Asia. Solid Earth, 5(1), 227-273. doi:10.5194/se-5-227-2014. The Cretaceous and Cenozoic tectonic evolution of Southeast Asia Download supplementary material – zip file

Geochemistry, Geophysics, Geosystems – Community infrastructure and repository for marine magnetic identifications

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magnetic_picks_globeMagnetic anomaly identifications form the primary data set from which the age of the oceanic lithosphere can be determined, a critical component of reconstructing the seafloor spreading history of ocean basins. This data is now available as part of an open source, community-driven online repository that contains quality-checked magnetic anomaly picks, organised by ocean basin and publication source.

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Geoscientific Model Development – A suite of early Eocene (~55 Ma) climate model boundary conditions

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Herold_etal_2014_BIOME4

Herold, N., Buzan, J., Seton, M., Goldner, A., Green, J. A. M., Müller, R. D., Markwick, P., & Huber, M. (2014). A suite of early Eocene (~ 55 Ma) climate model boundary conditions. Geoscientific Model Development, 7(5), 2077-2090. doi: 10.5194/gmd-7-2077-2014.

A suite of early Eocene (~ 55 Ma) climate model boundary conditions

Supplementary data

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Earth and Planetary Science Letters – Topographic assymetry of the South Atlantic from global models of mantle flow and lithospheric stretching

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Flament, N., Gurnis, M., Williams, S., Seton, M., Skogseid, J., Heine, C., & Müller, R. D. (2014). Topographic asymmetry of the South Atlantic from global models of mantle flow and lithospheric stretching. Earth and Planetary Science Letters, 387, 107-119. dx.doi.org/10.1016/j.epsl.2013.11.017. Topographic asymmetry of the South Atlantic from global models of mantle flow and lithospheric stretching … Read more…

Topographic asymmetry of the South Atlantic from global models of mantle flow and lithospheric stretching

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Flament et al EPSL 2014 - FigureCitation
Flament, N., Gurnis, M., Williams, S., Seton, M., Skogseid, J., Heine, C., & Müller, R. D. (2014). Topographic asymmetry of the South Atlantic from global models of mantle flow and lithospheric stretching. Earth and Planetary Science Letters, 387, 107-119. dx.doi.org/10.1016/j.epsl.2013.11.017.

Abstract
The relief of the South Atlantic is characterized by elevated passive continental margins along southern Africa and eastern Brazil, and by the bathymetric asymmetry of the southern oceanic basin where the western flank is much deeper than the eastern flank. We investigate the origin of these topographic features in the present and over time since the Jurassic with a model of global mantle flow and lithospheric deformation. The model progressively assimilates plate kinematics, plate boundaries and lithospheric age derived from global tectonic reconstructions with deforming plates, and predicts the evolution of mantle temperature, continental crustal thickness, long-wavelength dynamic topography, and isostatic topography. … Read more…

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Scientific Drilling – Exploring new drilling prospects in the Southwest Pacific

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Arculus, R., D’Hondt, S., Exon, N., Foster, C., Gallagher, S. J., Gurnis, M., … & Wallace, L. (2014). Exploring new drilling prospects in the Southwest Pacific. Scientific Drilling, 17, 45-50. doi: 10.5194/sd-17-45-2014. Exploring new drilling prospects in the southwest Pacific

Journal of Geodynamics – Geological, tomographic, kinematic and geodynamic constraints on the dynamics of sinking slabs

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Butterworth, N. P., Talsma, A. S., Müller, R. D., Seton, M., Bunge, H. P., Schuberth, B. S. A., … & Heine, C. (2014). Geological, tomographic, kinematic and geodynamic constraints on the dynamics of sinking slabs. Journal of Geodynamics, 73, 1-13. doi: 10.1016/j.jog.2013.10.006. Geological, tomographic, kinematic and geodynamic constraints on the dynamics of sinking slabs Supplementary material

Seawater chemistry driven by supercontinent assembly, breakup and dispersal, Müller et al. (2013)

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Muller etal Fig1 - Seawater Chemistry Driven by Supercontinental AssemblyCitation
Müller, R. D., Dutkiewicz, A., Seton, M. and Gaina, C. (2013). Seawater chemistry driven by supercontinent assembly, break-up and dispersal Geology. doi 10.1130/G34405.1.

Summary
Global oceans are known to have alternated between aragonite and calcite seas. These oscillations reflect changes in the Mg/Ca ratio of seawater, which control biomineralisation and the composition of marine carbonates and are thought to be caused by the time dependence of crustal accretion at mid-ocean ridge crests and associated high temperature mid-ocean ridge brine flux. Here we use global ocean basin reconstructions to demonstrate that these fluctuations are instead caused by the gradual growth and destruction of mid-ocean ridges and their relatively cool flanks during long-term tectonic cycles thus linking ocean chemistry to off-ridge low temperature hydrothermal flux. Early Jurassic aragonite seas were a consequence of supercontinent stability and minima in mid-ocean ridge length and basalt alteration. The break-up of Pangaea led to a gradual doubling in ridge length and a 50% increase in hydrothermal flux mainly through an enormous increase in ridge flank area, leading to enhanced alteration of basalt, lowered seawater Mg/Ca ratios and marine hypercalcification from 140 to 35 Ma. … Read more…

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Earth and Planetary Science Letters – Convergence of tectonic reconstructions and mantle convection models for significant fluctuations in seafloor spreading

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Coltice, N., Seton, M., Rolf, T., Müller, R. D., & Tackley, P. J. (2013). Convergence of tectonic reconstructions and mantle convection models for significant fluctuations in seafloor spreading. Earth and Planetary Science Letters, 383, 92-100. doi:10.1016/j.epsl.2013.09.032. Convergence of tectonic reconstructions and mantle convection models for significant fluctuations in seafloor spreading

Geology – Seawater chemistry driven by supercontinent assembly, breakup, and dispersal

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Müller, R. D., Dutkiewicz, A., Seton, M., & Gaina, C. (2013). Seawater chemistry driven by supercontinent assembly, breakup, and dispersal. Geology, 41(8), 907-910. doi: 10.1130/G34405.1. Seawater chemistry driven by supercontinent assembly, breakup, and dispersal

Earth Science Reviews – The tectonic evolution of the Arctic since Pangaea breakup: Integrating constraints from surface geology and geophysics with mantle structure

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Shephard, G. E., Müller, R. D., & Seton, M. (2013). The tectonic evolution of the Arctic since Pangea breakup: Integrating constraints from surface geology and geophysics with mantle structure. Earth-Science Reviews, 124, 148-183. doi:10.1.1016/j.earscirev.2013.05.012. The tectonic evolution of the Arctic since Pangea breakup: Integrating constraints from surface geology and geophysics with mantle structure

Earth and Planetary Science Letters – Organisation of the tectonic plates in the last 200 Myr

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Morra, G., Seton, M., Quevedo, L., & Müller, R. D. (2013). Organization of the tectonic plates in the last 200 Myr. Earth and Planetary Science Letters, 373, 93-101. doi:10.1016/j.epsl.2013.04.020. Organization of the tectonic plates in the last 200 Myr

The tectonic evolution of the Arctic since Pangea breakup: Integrating constraints from surface geology and geophysics with mantle structure

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Shephard Arctic IconCitation
Shephard, G. E., Müller, R. D., & Seton, M. (2013). The tectonic evolution of the Arctic since Pangea breakup: Integrating constraints from surface geology and geophysics with mantle structure. Earth-Science Reviews, 124, 148-183. doi:10.1016/j.earscirev.2013.05.012

Summary
The tectonic evolution of the circum-Arctic, including the northern Pacific, Siberian and North American margins, since the Jurassic has been punctuated by the opening and closing of ocean basins, the accretion of autochthonous and allochthonous terranes and associated deformation. This complexity is expressed in the uncertainty of plate tectonic models of the region, with the time-dependent configurations and kinematic history remaining poorly understood. … Read more…

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Towards community-driven paleogeographic reconstructions: integrating open-access paleogeographic and paleobiology data with plate tectonics

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PaleobioSummary
A variety of paleogeographic reconstructions have been published, with applications ranging from paleoclimate, ocean circulation and faunal radiation models to resource exploration; yet their uncertainties remain difficult to assess as they are generally presented as low-resolution static maps. We present a methodology for ground-truthing the digital Palaeogeographic Atlas of Australia by linking the GPlates plate reconstruction tool to the global Paleobiology Database and a Phanerozoic plate motion model.

We develop a spatio-temporal data mining workflow to validate the Phanerozoic Palaeogeographic Atlas of Australia with paleoenvironments derived from fossil data. … Read more…

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Biogeosciences – Towards community-driven paleogeographic reconstructions: integrating open-access paleogeographic and paleobiology data with plate tectonics

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Wright, N., Zahirovic, S., Müller, R. D., & Seton, M. (2013). Towards community-driven paleogeographic reconstructions: integrating open-access paleogeographic and paleobiology data with plate tectonics. Biogeosciences, 10(3), 1529-1541. doi:10.5194/bg-10-1529-2013. Towards community-driven paleogeographic reconstructions: integrating open-access paleogeographic and paleobiology data with plate tectonics

Global continental and ocean basin reconstructions since 200 Ma

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Plate reconstruction 200Ma-1Global plate motion models provide a spatial and temporal framework for geological data and have been effective tools for exploring processes occurring at the earth’s surface. However, published models either have insufficient temporal coverage or fail to treat tectonic plates in a self-consistent manner. They usually consider the motions of selected features attached to tectonic plates, such as continents, but generally do not explicitly account for the continuous evolution of plate boundaries through time. … Read more…

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Eastern Australasian Basins Symposium IV – Late Cretaceous to present-day opening of the southwest Pacific constrained by numerical models and seismic tomography

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Matthews, K. J., Seton, M., Flament, N., & Müller, R. D. (2012). Late Cretaceous to present-day opening of the southwest Pacific constrained by numerical models and seismic tomography. In Eastern Australasian Basins Symposium EABS IV: Exploration—Driving Future Energy Solutions, Petroleum Exploration Society of Australia (pp. 105-119). Download the paper – pdf

Eastern Australasian Basins Symposium IV – Subduction history in the Melanesian borderlands region, SW Pacific

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Seton, M., Flament, N., & Müller, R. D. (2012). Subduction history in the Melanesian Borderlands region, SW Pacific. In: Mares, T. (Ed), 2012. Eastern Australasian Basins Symposium IV. Petroleum Exploration Society of Australia, Special Publication, 1-12. Download the paper – pdf

Earth-Science Reviews – Global continental and ocean basin reconstructions since 200 Ma

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Seton, M., Müller, R. D., Zahirovic, S., Gaina, C., Torsvik, T., Shephard, G., … & Chandler, M. (2012). Global continental and ocean basin reconstructions since 200Ma. Earth-Science Reviews, 113(3), 212-270. doi:10.1016/j.earscirev.2012.03.002. Download the paper – pdf