HelioWebKF University of Graz, Institute of Earth Sciences
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I[KF University of Graz, Institute of Earth Sciences]
PI["Parent Institutions (1)"]
CI["Child Institutions (0)"]
AW["Affiliated Works (47)"]
CA["Linked Collaborating Authors (2)"]
I== skos:broader ==>PI
CI== skos:broader ==>I
AW== affil ==>I
AW== author ==>CA
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Parent Institutions [?]
Child Institutions [?]
Affiliated Works
sorted by decreasing year, and then by display-name
- Thermochronological Evolution of the Sierra Maestra, Cuba: Significance for Caribbean Tectonics
- Cenozoic Climate Evolution of Northeastern Tibet: Carbon and Oxygen Isotope Results From the Qaidam Basin, Western China
- Geodynamic evolution of an UHP Suture Zone in the Greek Rhodope
- Late Miocene Freshwater Runoff Seasonality Inferred by LA-ICP-MS and TIMS Analyses on Eastern Mediterranean Corals
- Thermocline-West African Monsoon-Coupling Recorded in Guinea Basin Sediments
- Comparison of single-continuum and hybrid flow models representing turbulent conduit flow in spring catchments (Invited)
- The abyssal SE - Atlantic: benthic foraminifers as oceanographic proxies
- Via GeoAlpina - an international project of IYPE (Invited)
- Water retention curves of loamy-sandy soils: Transient evaporation method versus steady-state tension and pressure techniques
- What does the early recession of spring hydrographs tell about aquifer properties? (Invited)
- Determining the rates of geological processes in a large-scale metamorphic complex: a multi-method approach
- Multi-proxy cross-calibration and validation of paleoenvironmental changes based on lake sediment records: A case study from the Tibetan Plateau
- A petrological study of Paleoarchean rocks of the Onverwacht Group: New insights into the geologic evolution of the Barberton Greenstone Belt, South Africa
- Metamorphic Evolution of Selected Pan-African Terrains across central Gondwana
- On the evolution of the Arabian-Nubian Shield and the largest shear zone on the Earth
- Solar Cycle Driven Environmental Changes on Decadal to Centennial Scale of Late Miocene Lake Sediments (tortonian, Lake Pannon, Central Europe)
- Benthic foraminiferal assemblages reveal the history of the Burdigalian Seaway
- Fe-dominated samarskite - a new member of the samarskite 'group'?
- Late Devonian Anoxia Events in the Central Asian Orogenic Belt: a Global Phenomenon
- Paratethys-Southern Ocean teleconnection in the mid-Burdigalian: European climate on the verge to the Miocene Climate Optimum
- Quantitative Pleistocene calcareous nannofossil biostratigraphy: preliminary results from the IODP Site U1385 (Exp 339), the Shackleton Site
- Strike-slip accommodated core complexes in the Najd fault system, Arabian-Nubian shield
- Late Pliocene History of Mediterranean Outflow Water in the Gulf of Cadiz (IODP Expedition 339, Site U1389)
- New Insights into the 8.2 ka Cold Event and Subsequent Climate Recovery in Central Europe Provided by a Precisely Dated Ostracod δ<SUP>18</SUP>O Record from Mondsee (Austria)
- Plume tectonics and cratons formation in the early Earth
- Indonesian Throughflow drove Australian climate from humid Pliocene to arid Pleistocene
- Linking changes in Indonesian Throughflow dynamics with the Middle Pleistocene Transition
- Palaeobathymetric Interpretations using Foraminiferal Data from the North-west Continental Shelf off Western Australia, IODP Expedition 356
- Plume-induced cratonization in Archean Earth
- Reconstructing initial Mediterranean Outflow from Benthic Foraminifera
- The Austrian network of isotopes in rivers: Long-term time series of isotopes in river water in Central Europe (1963-2015)
- Timing and pacing of Pliocene climate and paleoenvironmental change in southwestern Australia (IODP Exp. 356, Site U1459).
- Indian Ocean circulation changes over the Middle Pleistocene Transition.
- Late Pleistocene Age Model for Site U1460, Perth Basin, SW Australian Shelf: Implications for Leeuwin Current History
- Marine Isotope Stage (MIS) M2 ( 3.3 Ma) in the southern hemisphere: constraining the climatic drivers of a short-term glaciation event during the Pliocene warm Period.
- Post-magmatic structural evolution of the Troodos Ophiolite Pillow Lavas revealed by microthermometry within vein precipitates, with application to Alpine-Mediterranean supra-subduction zone settings
- Seamount subduction and serpentinite mud volcanisms in the Mariana convergent margin system: time constraints from micropaleontological studies (IODP Expedition 366)
- The Africa Initiative for Planetary and Space Sciences
- The Cocos Ridge hydrothermal system revealed by microthermometry of fluid and melt inclusions
- Dating serpentinite mud volcanism and seamount subduction in the Mariana convergent margin system (IODP Expedition 366)
- Did Indonesian Throughflow changes affect the MOC during the MPT? New data from the Eastern Indian Ocean
- Izu-Bonin forearc tectonics subsequent to Pacific Plate subduction initiation: resolving a 15 Ma hiatus enigma
- Tasman Leakage: the missing link in AMOC
- Indonesian Throughflow and Leeuwin Current dynamics in the Plio-Pleistocene
- Post-magmatic Fluid Flow and Vein Mineralization in Supra-subduction Zones: A Comparative Study from the Troodos Ophiolite and the Izu-Bonin Forearc and Rear Arc
- Serpentinite Mud Volcanism and Exhumation of Forearc- and Lower Plate Material in the Mariana Convergent Margin System (IODP Expedition 366)
- Subannual record of climate change in Lake Malawi