Glen Phillips

Philips (Finland)

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Solveig Estrada

Federal Institute for Geosciences and Natural Resources

Andreas Läufer

Federal Institute for Geosciences and Natural Resources

Friedhelm Henjes‐Kunst

Federal Institute for Geosciences and Natural Resources

Jürgen Koepke

Leibniz University Hannover

Karsten Piepjohn

Federal Institute for Geosciences and Natural Resources

Dominique Kosanke

Meinhard Classen

Technical University of Munich

Thomas Röesch

Universität Hamburg

Peter Born

German Sport University Cologne

N. Weigert

Barmherzige Brüder Klinikum St. Elisabeth in Straubing

Cooperative Institutions

Technical University of Munich

Indiana University – Purdue University Indianapolis

Monash University

Klinikum rechts der Isar

University of Melbourne

Indiana University School of Medicine

Geological Survey of Western Australia

University Medical Center

University Hospital and Clinics

Federal Institute for Geosciences and Natural Resources

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The tectonic history of the Ruker Province, southern Prince Charles Mountains, East Antarctica: implications for Gondwana and Rodinia

Glen Phillips

Rodinia

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Citations (2)

Value of double-brush cytology and stricture dilation in the evaluation of malignant biliary obstruction

Gastrointestinal Endoscopy (2001)

Evan L. Fogel Stuart Sherman James L. Watkins Lois Bucksot Ann Lee

Dilation (metric space)

Value (mathematics)

10.1016/s0016-5107(01)80143-7

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Citations (2)

Constraining regional scale fault architecture in the southern New England Orogen: integration of seismic, multiscale edges and surface mapping

ASEG Extended Abstracts (2015)

Jamie A. Robinson Glen Phillips Lisa Nix

Regional scale fault structures are considered a first order control on hydrothermal ore systems. Recognition and delineation of such features is essential for search space reduction and project selection in exploration. The New England Orogen in northeastern New South Wales has significant potential for the discovery of new hydrothermal ore systems. However, limits to interpretation of broad scale geophysics in the region and limited exposure for ground-based mapping have hampered the recognition of the first order fault architecture in many areas.As part of the Geological Survey of New South Wales 3D mapping program, we aim to further the understanding of strike extensive and depth penetrative regional scale fault architecture in the southern New England Orogen. The workflow for constraining the regional 3D fault architecture involves integrating a limited number of deep seismic lines with broader gravity and magnetic wavelet-based multiscale edges. All the geophysical data sets are further constrained by the Geological Survey of New South Wales’ seamless geology mapping and surface structural orientation data. The work to date demonstrates correlation between the lateral position of multiscale edges and their dip inferred from upward continuation, with steeper dipping structures interpreted in seismic lines. Strike orientations of edges, or systematic breaks in edges, are broadly consistent with structural orientations previously recognised in mapping, but often not at the true regional scale as suggested by edge continuity. Known hydrothermal ore systems in the southern New England Orogen display a strong correlation with the deeply penetrating edges.

Geologic map

10.1071/aseg2015ab174

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Thermochronological (⁴⁰Ar/³⁹Ar) evidence of Early Palaeozoic basin inversion within the southern Prince Charles Mountains, East Antarctica: implications for East Gondwana

Figshare (2016)

Glen Phillips Christopher J.L. Wilson David Phillips Stan K. Szczepanski

⁴⁰Ar/³⁹Ar systematics within metasedimentary rocks exposed in the southern Prince Charles Mountains, East Antarctica, were thermally reset during a period of Early Palaeozoic (between 524 ± 1 Ma and 486 ± 2 Ma) orogenesis. This event affected three temporally distinct (Archaean to Neoproterozoic) stratigraphic levels that are now exposed in the upper crust. In the structural record, evidence of orogenesis during Early Palaeozoic times is preserved as late-stage, subvertical mylonite zones in the Archaean orthogneiss–metasedimentary basement and thin-skinned folding and thrusting of the overlying Neoproterozoic metasedimentary rocks. Synchronous cooling ages, contrasting structural styles and similar peak metamorphic conditions are interpreted as reflecting basement-involved thin-skinned deformation that was the result of inversion of a Neoproterozoic basin. The presence of pre-existing crustal heterogeneities is the mechanism that localized Early Palaeozoic orogenesis within the region. This interpretation differs from previous models that attribute Early Palaeozoic orogenesis within the southern Prince Charles Mountains to a collisional tectonic setting. An Early Palaeozoic intra-cratonic setting for the region suggests that amalgamation between India and Antarctica was likely to have occurred prior to the final construction of Gondwana.

10.6084/m9.figshare.3454400

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Three-dimensional inversion modelling of a Neoproterozoic basin in the southern Prince Charles Mountains, East Antarctica

Tectonophysics (2008)

M. A. McLean Tim Rawling Peter Betts Glen Phillips Chris Wilson

10.1016/j.tecto.2008.04.023

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Citations (27)

Thermochronological ( ⁴⁰ Ar/ ³⁹ Ar) evidence of Early Palaeozoic basin inversion within the southern Prince Charles Mountains, East Antarctica: implications for East Gondwana

Journal of the Geological Society (2007)

Glen Phillips Christopher J.L. Wilson David Phillips Stan K. Szczepanski

40 Ar/ 39 Ar systematics within metasedimentary rocks exposed in the southern Prince Charles Mountains, East Antarctica, were thermally reset during a period of Early Palaeozoic (between 524 ± 1 Ma and 486 ± 2 Ma) orogenesis. This event affected three temporally distinct (Archaean to Neoproterozoic) stratigraphic levels that are now exposed in the upper crust. In the structural record, evidence of orogenesis during Early Palaeozoic times is preserved as late-stage, subvertical mylonite zones in the Archaean orthogneiss–metasedimentary basement and thin-skinned folding and thrusting of the overlying Neoproterozoic metasedimentary rocks. Synchronous cooling ages, contrasting structural styles and similar peak metamorphic conditions are interpreted as reflecting basement-involved thin-skinned deformation that was the result of inversion of a Neoproterozoic basin. The presence of pre-existing crustal heterogeneities is the mechanism that localized Early Palaeozoic orogenesis within the region. This interpretation differs from previous models that attribute Early Palaeozoic orogenesis within the southern Prince Charles Mountains to a collisional tectonic setting. An Early Palaeozoic intra-cratonic setting for the region suggests that amalgamation between India and Antarctica was likely to have occurred prior to the final construction of Gondwana.

10.1144/0016-76492006-073

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Citations (69)

Long distance transport of eclogite and blueschist during early Pacific Ocean subduction rollback

EGUGA (2017)

Renée Tamblyn Martin Hand David E. Kelsey Glen Phillips Robert Anczkiewicz

Blueschist

Rollback

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MRCP versus ERCP in the evaluation of patients with suspected biliopancreatic disease — Can ERCPS be saved?