Prof Dietmar Müller

Dietmar MüllerGroup Coordinator

dietmar.muller@sydney.edu.au

Phone: +61 2 9351 4255
Fax: +61 2 9351 3644

Madsen Building F09, Room 406
School of Geosciences
The University of Sydney
Sydney, NSW 2006
Australia

View Dietmar's Sydney Uni page

See below for EarthByte content related to Dietmar.

ScienceNews features an article on Pacific plate motions paper

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EarthByte paper ‘Revision of Paleogene plate motions in the Pacific and implications for the Hawaiian-Emperor bend‘ is featured in ScienceNews with an article entitled ‘Plate loss gave chain of Pacific islands and seamounts a bend‘. Revision of Paleogene plate motions in the Pacific and implications for the Hawaiian-Emperor bend

Global plate and continental velocities since Pangea breakup

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This animation portrays the motion of continents (grey, yellow, orange and red) and oceanic plates (blue) since Pangea breakup from 200 million years ago. The model is a modified version of the Seton et al.Citation Zahirovic, S., R. Müller, M. Seton, and N. Flament (2015), Tectonic speed limits from plate kinematic reconstructions, Earth and Planetary … Read more…

Geophysical Research Letters – Ridge subduction sparked reorganisation of the Pacific plate-mantle system 60-50 million years ago

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Seton, M., Flament, N., Whittaker, J., Müller, R. D., Gurnis, M., & Bower, D. J. (2015). Ridge subduction sparked reorganization of the Pacific plate‐mantle system 60–50 million years ago. Geophysical Research Letters, 42(6), 1732-1740. doi: 10.1002/2015GL063057. Ridge subduction sparked reorganization of the Pacific plate‐mantle system 60–50 million years ago

A tectonic model reconciling evidence for the collisions between India, Eurasia and intra-oceanic arcs of the central-eastern Tethys

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Gibbons etal AgeGrid Vels MagPicks v3 0175Citation
Gibbons, A., Zahirovic, S., Muller, R.D., Whittaker, J., and Yatheesh, V. 2015. A tectonic model reconciling evidence for the collisions between India, Eurasia and intra-oceanic arcs of the central-eastern Tethys. Gondwana Research FOCUS, doi: 10.1016/j.gr.2015.01.001.

Summary
Despite several decades of investigations, inferences on the timing and nature of collisions along the Mesozoic–Cenozoic Eurasian margin remain controversial. We assimilate geological and geophysical evidence into a plate tectonic model for the India–Eurasia collision that includes continuously– … Read more…

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Ore Geology Reviews – Prospectivity of Western Australian iron ore from geophysical data using a reject option classifier

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Merdith, A. S., Landgrebe, T. C., & Müller, R. D. (2015). Prospectivity of Western Australian iron ore from geophysical data using a reject option classifier. Ore Geology Reviews. doi: 10.1016/j.oregeorev.2015.03.014. Prospectivity of Western Australian iron ore from geophysical data using a reject option classifier

Geology – Revision of Paleogene plate motions in the Pacific and implications for the Hawaiian-Emperor bend

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Wright, N. M., Müller, R. D., Seton, M., & Williams, S. E. (2015). Revision of Paleogene plate motions in the Pacific and implications for the Hawaiian-Emperor bend. Geology, 43(5), 455-458. doi: 10.1130/G36303.1. Revision of Paleogene plate motions in the Pacific and implications for the Hawaiian-Emperor bend

Earth and Planetary Science Reviews – Absolute plate motions since 130 ma constrained by subduction zone kinematics

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Williams, S., Flament, N., Müller, R. D., & Butterworth, N. (2015). Absolute plate motions since 130 Ma constrained by subduction zone kinematics. Earth and Planetary Science Letters, 418, 66-77. doi:10.1016/j.epsl.2015.02.026. Absolute plate motions since 130 Ma constrained by subduction zone kinematics

Age, spreading rates and spreading asymmetry of the world’s ocean crust

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agegrid_ageerror_2008 rategrid_asymgrid_2008We present four companion digital models of the age, age uncertainty, spreading rates and spreading asymmetries of the world’s ocean basins as geographic and Mercator grids with 2 minute resolution. The grids include data from all the major ocean basins as well as detailed reconstructions of back-arc basins.

The age, spreading rate and asymmetry at each grid node is determined by linear interpolation between adjacent seafloor isochrons in the direction of spreading. Ages for ocean floor between the oldest identified magnetic anomalies and continental crust are interpolated by geological estimates of the ages of passive continental margin segments. … Read more…

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Supplementary resources for “Absolute plate motions since 130 Ma constrained by subduction zone kinematics”

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Williams et al 2015 figure 3Citation
Williams, S., Flament, N., Müller, R. D., & Butterworth, N. (2015). Absolute plate motions since 130 Ma constrained by subduction zone kinematics. Earth and Planetary Science Letters, 418, 66-77. doi:10.1016/j.epsl.2015.02.026.

Summary
The supplementary data set comprise plate reconstructions from 130 Ma to present-day, designed to be used within the open-source reconstruction software GPlates.

There are eight sets of reconstructions. In each case, the relative plate motion (RPM) model is unchanged; the differences lie in the absolute plate motion (APM) model. This is expressed in the rotation file as the finite poles of rotation that describe motion of Africa relative to the Earth’s spin-axis. These files were the basis of the results presented in the EPSL paper.  … Read more…

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Supplementary resources for "Absolute plate motions since 130 Ma constrained by subduction zone kinematics"

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Williams et al 2015 figure 3Citation
Williams, S., Flament, N., Müller, R. D., & Butterworth, N. (2015). Absolute plate motions since 130 Ma constrained by subduction zone kinematics. Earth and Planetary Science Letters, 418, 66-77. doi:10.1016/j.epsl.2015.02.026.

Summary
The supplementary data set comprise plate reconstructions from 130 Ma to present-day, designed to be used within the open-source reconstruction software GPlates.

There are eight sets of reconstructions. In each case, the relative plate motion (RPM) model is unchanged; the differences lie in the absolute plate motion (APM) model. This is expressed in the rotation file as the finite poles of rotation that describe motion of Africa relative to the Earth’s spin-axis. These files were the basis of the results presented in the EPSL paper.  … Read more…

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Earth and Planetary Science Letters – Tectonic speed limits from plate kinematic reconstructions

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Zahirovic, S., Müller, R. D., Seton, M., & Flament, N. (2015). Tectonic speed limits from plate kinematic reconstructions. Earth and Planetary Science Letters, 418, 40-52. doi: 10.1016/j.epsl.2015.02.037. Tectonic speed limits from plate kinematic reconstructions

Australian Journal of Earth Sciences – Evaluating global paleoshoreline models for the Cretaceous and Cenozoic

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Heine, C., Yeo, L. G., & Müller, R. D. (2015). Evaluating global paleoshoreline models for the Cretaceous and Cenozoic. Australian Journal of Earth Sciences, (ahead-of-print), 1-13. Evaluating global paleoshoreline models for the Cretaceous and Cenozoic Download the Paleocoastline files – zip file

Australian Journal of Earth Sciences – Uncovering the relationship between subducting bathymetric ridges and volcanic chains with significant earthquakes using geophysical data mining

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Landgrebe, T. C. W., & Müller, R. D. (2015). Uncovering the relationship between subducting bathymetric ridges and volcanic chains with significant earthquakes using geophysical data mining. Australian Journal of Earth Sciences, 62(2), 171-180. doi: 10.1080/08120099.2015.1003145. Uncovering the relationship between subducting bathymetric ridges and volcanic chains with significant earthquakes using geophysical data mining

Earth-Science Reviews – Geological and kinematic constraints on late Cretaceous to mid Eocene plate boundaries in the Southwest Pacific

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Matthews, K. J., Williams, S. E., Whittaker, J. M., Müller, R. D., Seton, M., & Clarke, G. L. (2015). Geologic and kinematic constraints on Late Cretaceous to mid Eocene plate boundaries in the southwest Pacific. Earth-Science Reviews, 140, 72-107. doi: 10.1016/j.earscirev.2014.10.008. Geologic and kinematic constraints on Late Cretaceous to mid Eocene plate boundaries in the southwest … Read more…

The Basin GENESIS Hub

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Basin GENESIS Hub logo

The ARC Research Hub for Basin Geo-dynamics and Evolution of Sedimentary Systems (Basin Genesis Hub, BGH) brings together a broad range of expertise for the development and application of cutting-edge numerical modelling tools with the aim of improving the understanding of the formation and evolution of basins. The coupling of the evolution of mantle flow, … Read more…

The Virtual Geological Observatory: a 4D view into the earth through deep-time data-mining (VIRGO)

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Presentations Image

Project Summary
Australian Laureate Fellow Prof. Dietmar Müller and the EarthByte Group within the University of Sydney’s School of Geosciences are embarking on an ambitious new research program: building a Virtual Geological Observatory.

Fifty percent of Australia’s export income comes from the minerals and energy sector. Over three-quarters of these exports come from deposits discovered prior to 1980. … Read more…

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The Virtual Observatory: Deep time travel in the Pacific, presented by Dietmar Müller

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Deep Time Travel — it’s not just science fiction! The EarthByte Group is developing an Experimental Virtual Planet to explore Earth’s geological evolution, enabling deep time travel from your own laptop, anywhere, anytime, and all without a police box. In this illustrated talk, Australian Laureate Fellow Professor Dietmar Müller reports on the experimental work of … Read more…

Science – New global marine gravity model from Cryo-Sat-2 and Jason-1 reveals buried tectonic structure

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Sandwell, D. T., Müller, R. D., Smith, W. H., Garcia, E., & Francis, R. (2014). New global marine gravity model from CryoSat-2 and Jason-1 reveals buried tectonic structure. science, 346(6205), 65-67. doi: 10.1126/science.1258213.

New global marine gravity model from CryoSat-2 and Jason-1 reveals buried tectonic structure

Download supplementary material – pdf

… Read more…

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New global marine gravity model, Sandwell et al. (2014)

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Indian Ocean View Westward from AustraliaCitation
Sandwell, D. T., Müller, R. D., Smith, W. H. F., Garcia, E. and Francis, R. 2014. New global marine gravity model from Cryo-Sat-2 and jason-1 reveals buried tectonic structure. Science, Vol. 346, 6205, pp. 65-67, doi: 10.1126/science.1258213.

Summary
New global marine gravity model from CryoSat-2 and Jason-1 reveals buried tectonic structure.

View the new gravity map in an online 3D portal!

Gravity models are powerful tools for mapping tectonic structures, especially in the deep ocean basins where the topography remains unmapped by ships or is buried by thick sediment. We combined new radar altimeter measurements from satellites CryoSat-2 and Jason-1 with existing data to construct a global marine gravity model that is two times more accurate than previous models. We found an extinct spreading ridge in the Gulf of Mexico, a … Read more…

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Post-Jurassic tectonic evolution of southeast Asia from Zahirovic et al. (2014)

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Asia Zahirovic 20maCitation
Zahirovic, S., Seton, M., and Müller, R. D., (2014). The Cretaceous and Cenozoic tectonic evolution of Southeast Asia: Solid Earth (EGU).

Summary
Tectonic reconstructions of Southeast Asia have given rise to numerous controversies that include the accretionary history of Sundaland and the enigmatic tectonic origin of the Proto South China Sea. We assimilate a diversity of geological and geophysical observations into a new regional plate model, coupled to a global model, to address these debates.

Our approach takes into account terrane suturing and accretion histories, the location of subducted slabs imaged in mantle tomography in order to constrain the evolution of regional subduction zones, as well as plausible absolute and relative plate velocities and tectonic driving mechanisms. … Read more…

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The tectonic stress field evolution of India since the Oligocene

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Muller etal India Paleostress Graphical AbstractCitation
Müller, R. D., Yatheesh, V., & Shuhail, M. (2014). The tectonic stress field evolution of India since the Oligocene. Gondwana Research.

Summary
We use a 2 dimensional finite element model with heterogeneous elastic strengths in continental areas to model the regional stress field orientation and relative magnitudes in and around India for 33 Ma, 20 Ma and the present day. The large-scale geological structure of India is embedded in our model by using published outlines of cratons, fold belts and basins, associated with estimates of their relative strengths, enabling the modelling of stress field deflections along interfaces between relatively strong and weak tectonic elements through time. … Read more…

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EarthByte Group makes the finals of the Eureka Prize

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The EarthByte group is a finalist for the Eureka Prize from the Australian Museum, for its development of GPlates software! The prize is awarded annually for research innovation and GPlates was nominated for providing a “experimental virtual planet” to investigate geological systems through deep time. You can read more about the Eureka Prize here. Watch the … Read more…

Solid Earth – Pacific plate slab pull and intraplate deformation in the early Cenozoic

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Butterworth, N. P., Müller, R. D., Quevedo, L., O’Connor, J. M., Hoernle, K., & Morra, G. (2014). Pacific Plate slab pull and intraplate deformation in the early Cenozoic. Solid Earth, 5(2). doi: 10.5194/se-5-757-2014. Pacific Plate slab pull and intraplate deformation in the early Cenozoic

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

Integrating deep-Earth and surface processes for frontier-basin exploration

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Project Summary
Sea level has changed by up to 300m through geological time. These fluctuations, caused by plate tectonics and convection in the Earth’s mantle, have created vast sedimentary basins and associated resources such as petroleum, natural gas and coal.

In this project, we propose to bring together global 4D databases with cutting-edge 3D numerical simulations to reconstruct how mid-ocean ridge creation and the recycling of old, cold oceanic plates into the mantle have driven surface topography and sea-level change globally since the breakup of the super-continent Pangaea. … Read more…

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