Results 171 to 180 of about 7,236 (215)
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Late Paleozoic Tectonic Analysis and Geochronology Study by Shrimp Zircon U-Pb Dating
Chemistry and Technology of Fuels and Oils, 2019Sinkiang Hami Redstone Copper in China is a super-large volcanic hydrothermal deposit formed as a result of multi-stage secondary tectonic activity in the Hercynian period of tectonic movement. In this work, we have studied the effect of the geomechanical nature on the structure of faults stretched in different directions and have studied the age of ...
Dongyu Li +4 more
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The contribution of the sensitive high-resolution ion microprobe (SHRIMP) to lunar geochronology
Precambrian Research, 2010Abstract The sensitive high-resolution ion microprobe (SHRIMP) developed at the Australian National University (ANU) was the first of the high-resolution ion microprobes. The impact of this instrument on geochronological research over the last twenty years has been immense.
Pidgeon, Robert +2 more
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SHRIMP U–Pb geochronology from Mount Kirkby, northern Prince Charles Mountains, East Antarctica
Antarctic Science, 2000Sensitive High Resolution Ion MicroProbe (SHRIMP) U–Pb zircon dating of pegmatites from Mount Kirkby, northern Prince Charles Mountains, east Antarctica indicates felsic intrusive activity at 991 ± 22 Ma and 910 ± 18 Ma. Pegmatite emplacement occurred during prolonged high-grade early Neoproterozoic tectonism.
C.J. Carson +4 more
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Journal of the Geological Society, 1995
SHRIMP U-Pb zircon ages have been obtained for a sample of metasedimentary gneiss from the Smallefjord sequence in the NE Greenland Caledonides. Pre-1000 Ma zircons are interpreted as being detrital in origin; the source region contained late Archaean rocks (or younger sediments or inheritance-rich granites derived from them) and several ...
R. A. STRACHAN +2 more
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SHRIMP U-Pb zircon ages have been obtained for a sample of metasedimentary gneiss from the Smallefjord sequence in the NE Greenland Caledonides. Pre-1000 Ma zircons are interpreted as being detrital in origin; the source region contained late Archaean rocks (or younger sediments or inheritance-rich granites derived from them) and several ...
R. A. STRACHAN +2 more
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SHRIMPDB: a new geoanalytical database for U-Th-Pb geochronological data from SHRIMP measurements
Earth Science Informatics, 2018This paper introduces a novel web-based database, SHRIMPDB, to support the efficient reutilization of U-Th-Pb geochronological data from sensitive high-resolution ion microprobe (SHRIMP) measurements. In order to provide complete data content that can be reutilized by Earth scientists, a new data model containing analytical data and relevant sample ...
Yutong He +5 more
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SHRIMP U-Pb Geochronology of the Closepet Granite and Peninsular Gneiss, Karnataka, South India
Journal Geological Society of India, 1991Abstract Zircons separated from a sample of Peninsular gneiss (82-KD 14) from Kabbaldurga quarry, and a homogeneous Closepet granite (KO84-13) from near Ramnagaram have been dated with the ion microprobe SHRIMP. The Peninsular gneiss sample, a metatexite, contains an arrested charnockite transition and constitutes an amphibolite ...
C. R. L. Friend, A. P. Nutman
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SHRIMP U–Pb geochronology of authigenic xenotime and its potential for dating sedimentary basins
Australian Journal of Earth Sciences, 2000SHRIMP (Sensitive High‐Resolution Ion MicroProbe) analytical procedures have been developed to enable dating of the small, early diagenetic xenotime overgrowths that commonly occur on zircons in siliciclastic sedimentary rocks. The method will be particularly useful in Precambrian terranes, where diagenetic xenotime dating could play a role equivalent ...
I. R. Fletcher +2 more
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The Journal of Geology, 2001
Mesoproterozoic intrusive and granulite-grade metamorphic rocks in southern California have been inferred to be exotic to North America on the basis of perceived chronologic incompatibility with autochthonous cratonal rocks. Ion microprobe geochronology indicates that zircons in granulite-grade gneisses, dated at 1.4 Ga using conventional methods, are ...
Barth, A.P., Wooden, J.L., Coleman, D.S.
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Mesoproterozoic intrusive and granulite-grade metamorphic rocks in southern California have been inferred to be exotic to North America on the basis of perceived chronologic incompatibility with autochthonous cratonal rocks. Ion microprobe geochronology indicates that zircons in granulite-grade gneisses, dated at 1.4 Ga using conventional methods, are ...
Barth, A.P., Wooden, J.L., Coleman, D.S.
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Precambrian Research, 2009
The Pine Creek Orogen, located on the exposed northern periphery of the North Australian Craton, comprises a thick succession of variably metamorphosed Palaeoproterozoic siliciclastic and carbonate sedimentary and volcanic rocks, which were extensively intruded by mafic and granitic rocks.
Julie A. Hollis +2 more
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The Pine Creek Orogen, located on the exposed northern periphery of the North Australian Craton, comprises a thick succession of variably metamorphosed Palaeoproterozoic siliciclastic and carbonate sedimentary and volcanic rocks, which were extensively intruded by mafic and granitic rocks.
Julie A. Hollis +2 more
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International Geology Review, 1998
U/Pb zircon ages of six rock units from southernmost Brazil were obtained by means of SHRIMP II techniques. The studied rocks occur on either side of the Neoproterozoic contact between a juvenile accreted terrane (the Vila Nova Terrane) and a crustal-reworked belt (the Dom Feliciano Belt).
Jayme A. D. Leite +3 more
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U/Pb zircon ages of six rock units from southernmost Brazil were obtained by means of SHRIMP II techniques. The studied rocks occur on either side of the Neoproterozoic contact between a juvenile accreted terrane (the Vila Nova Terrane) and a crustal-reworked belt (the Dom Feliciano Belt).
Jayme A. D. Leite +3 more
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