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Martin Danišík
Curtin University
GeomorphologyGeologyThermochronologyZirconFission track dating
122Publications
22H-index
1,458Citations
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Publications 70
Newest
#1Christopher L. Kirkland (Curtin University)H-Index: 35
#2Martin Danišík (Curtin University)H-Index: 22
Last. Lin Sutherland (Australian Museum)H-Index: 4
view all 6 authors...
Abstract U-Pb geochronology of Quaternary zircon crystals is challenging due to their low levels of radiogenic-Pb, the importance of accurate common-Pb correction, and the potential need for secular disequilibrium correction. (U-Th)/He dating offers an independent benchmark for the quality of U-Pb data and their reduction, including the various corrections, as the closure temperature of the He system in zircon is 900°C. Hence, U-Pb ages must predate (U-Th)/He ages, or at least be equal to them i...
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#1Hisatoshi Ito (CRIEPI: Central Research Institute of Electric Power Industry)H-Index: 13
#2Martin Danišík (Curtin University)H-Index: 22
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#1Christopher L. Kirkland (Curtin University)H-Index: 35
#2Milo Barham (Curtin University)H-Index: 6
Last. Martin Danišík (Curtin University)H-Index: 22
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Abstract In this work we present a novel zircon triple-dating approach (Lu-Hf – U-Pb – (U-Th)/He), complimented with grain shape and trace element chemistry to test models of trans-continental transport of ultimately Gondwana interior derived detritus. Our integrated fingerprinting approach on single zircon grains provides the opportunity for robust source correlations as each isotopic system provides temporal constraints on distinct geological processes, ranging from source age (Lu-Hf), through...
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Abstract Kyra is an important tephra unit for Nisyros pre-caldera stage due to a number of subunits with various compositions (basaltic andesite to dacite) and distal dispersion on surrounding Greek islands (Tilos and Chalki) and Datca peninsula (Turkey). As for the most Nisyros tephra units, the available radiometric ages of Kyra tephra are not compatible with the relatively well-established Nisyros tephrostratigraphy. This beclouds the characterization of both proximal and distal Kyra tephra a...
1 CitationsSource
#1Huan Li (CSU: Central South University)H-Index: 13
#2Martin Danišík (Curtin University)H-Index: 22
Last. Jing-Hua Wu (China University of Geosciences)H-Index: 7
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Abstract Low-temperature Sb (Au–Hg) deposits in South China account for more than 50% of the world’s Sb reserves, however, their genesis remains controversial. Here we report the first study that integrates U–Pb and Lu–Hf analysis by LA-(MC)-ICPMS and conventional (U–Th)/He analysis, all applied to single zircon crystals, in an attempt to constrain the origin and timing of world-class Sb (Au–Hg) deposits in Banxi (South China). Zircon separated from a quartz-stibnite ore and an altered country r...
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#1Gökhan AtıcıH-Index: 1
#2Axel K. Schmitt (Heidelberg University)H-Index: 46
Last. Hao-Yang Lee (AS: Academia Sinica)H-Index: 2
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Acigol volcanic complex is a bimodal volcanic field located at the western margin of the Neogene–Quaternary Cappadocian volcanic province in Central Anatolia (Turkey). Its most voluminous eruptions are preserved as a pair of widespread tuffs known as Lower Acigol Tuff (LAT) and Upper Acigol Tuff (UAT). Both are nearly aphyric high-silica rhyolites that are compositionally identical; they can be distinguished, however, by the presence of obsidian lithics in UAT and the absence thereof in LAT. Her...
2 CitationsSource
#1MingJian Cao (CAS: Chinese Academy of Sciences)H-Index: 16
#2Noreen J. Evans (Curtin University)H-Index: 27
Last. Brent I.A. McInnes (Curtin University)H-Index: 24
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#1Ni Tao (Chang'an University)H-Index: 2
#2Zheng-Xiang Li (ARC: Australian Research Council)H-Index: 74
Last. Yi-Gang Xu (CAS: Chinese Academy of Sciences)H-Index: 55
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Abstract The flat-slab subduction model has been proposed to explain the complex Mesozoic–Cenozoic geotectonic record of SE China as part of the Western Pacific margin. Here we investigate the post-250 Ma thermal history of the Shaoguan-Longnan region to evaluate the time-temperature evolution of local sedimentary and magmatic rocks in the context of the flat-subduction model. Our multi-chronological approach includes zircon U-Pb geochronology, 40Ar/39Ar dating of K-feldspar and biotite, (U-Th)/...
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#1Stijn Glorie (University of Adelaide)H-Index: 17
#2A. Otasevic (University of Adelaide)
Last. Wenjiao Xiao (CAS: Chinese Academy of Sciences)H-Index: 60
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Abstract The Junggar Alatau forms the northern extent of the Tian Shan within the Central Asian Orogenic Belt (CAOB) at the border of SE Kazakhstan and NW China. This study presents the Palaeozoic–Mesozoic post-collisional thermo-tectonic history of this frontier locality using an integrated approach based on three apatite geo-/thermochronometers: apatite U–Pb, fission track and (U–Th)/He. The apatite U–Pb dates record Carboniferous–Permian post-magmatic cooling ages for the sampled granitoids, ...
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#1Milo Barham (Curtin University)H-Index: 6
#2Christopher L. Kirkland (Curtin University)H-Index: 35
Last. Martin Danišík (Curtin University)H-Index: 22
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Abstract Detrital zircon U/Pb geochronology is a common tool used to resolve stratigraphic questions, inform basin evolution and constrain regional geological histories. In favourable circumstances, detrital zircon populations can contain a concomitant volcanic contribution that provides constraints on the age of deposition. However, for non-volcanic settings, proving isolated detrital zircon grains are from contemporaneous and potentially remote volcanism is challenging. Here we use same grain ...
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