Results 1 to 10 of about 6,544,459 (237)
Increased precision in isotope-dilution thermal ionization mass spectrometry (ID-TIMS) U–Pb geochronology has revealed age complexities in zircon populations that require new tools for understanding how the growth of zircon is related to geologic processes.
Schoene, B. +3 more
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U-Pb age of the Baltoro granite, northwest Himalaya, and implications for monazite U-Pb systematics
Geology, 1989The Baltoro granite is a major late- to post-tectonic plutonic phase of the Karakoram batholith of the northwest Himalaya in northern Pakistan. U-Pb zircon analyses indicate both emplacement at 21.0 ±0.5 Ma and significant Precambrian zircon inheritance.
Randall R. Parrish, Rein Tirrul
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, 2020
Spodumene and other pegmatites in the Lijiagou area are located in the central Songpan-Garze Fold Belt (SGFB), West Sichuan. These pegmatites are hosted within the giant Songpan-Garze polymetallic belt.
Guangchun Fei +10 more
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Spodumene and other pegmatites in the Lijiagou area are located in the central Songpan-Garze Fold Belt (SGFB), West Sichuan. These pegmatites are hosted within the giant Songpan-Garze polymetallic belt.
Guangchun Fei +10 more
semanticscholar +1 more source
Staurolite as an isotopic U–Pb geochronometer
Geology of Ore Deposits, 2016A new approach is suggested for measuring the real U–Pb and Pb–Pb ages of rock-forming metamorphic staurolite. Previously, two approaches have been used for this purpose: (1) measurement of the lead isotopic compositions, uranium and lead contents in leach substance as a product of the step-leaching technique; age is calculated by plotting the Pb–Pb ...
L. K. Levskii, A. F. Lobikov
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Interpretation of discordant U‐Pb zircon ages: An evaluation
Journal of Metamorphic Geology, 1997The most widely used technique for the determination of high precision mineral growth ages in igneous and metamorphic rocks is dating of zircons with the U‐Pb method. The interpretation of these ages, particularly in metamorphic settings, is hampered by an incomplete understanding of the common phenomenon of partial Pb‐loss in zircon.
Mezger, Klaus, KROGSTAD, E. J.
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SA01 – A Proposed Zircon Reference Material for Microbeam U‐Pb Age and Hf‐O Isotopic Determination
Geostandards and Geoanalytical Research, 2019A new natural zircon reference material SA01 is introduced for U‐Pb geochronology as well as O and Hf isotope geochemistry by microbeam techniques. The zircon megacryst is homogeneous with respect to U‐Pb, O and Hf isotopes based on a large number of ...
Chao Huang +14 more
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U-Pb AGE OF THE CHATTANOOGA SHALE
Geological Society of America Bulletin, 1960An attempt was made to date the upper black unit of the Gassaway member of the Chattanooga shale which carries the maximum U/Pb ratio. Three samples were analyzed by isotopic dilution techniques. The U238-Pb206 ages on all 3 samples agreed within their experimental errors. The average of the two samples with reasonably small errors gave an apparent age
J. C. COBB, J. L. KULP
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Air abrasion experiments in U-Pb dating of zircon
Chemical Geology, 1986Abstract Air abrasion of zircon grains can remove metamict material that has lost radiogenic Pb and zircon overgrowths that were added during younger events and thereby improve the precision of the age measurements and permit closer estimates of the original age.
S.S. Goldich, Lynn B. Fischer
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, 2020
Direct dating of W and W Sn deposits by wolframite is more reliable relatively to gangue mineral and important for understanding their timing and genesis. However, such analysis still lacks of homogeneous wolframite standard recently.
Yanwen Tang +6 more
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Direct dating of W and W Sn deposits by wolframite is more reliable relatively to gangue mineral and important for understanding their timing and genesis. However, such analysis still lacks of homogeneous wolframite standard recently.
Yanwen Tang +6 more
semanticscholar +1 more source
Chemical Geology, 1992
Four forms of the three-dimensional UPb method established so far are physically generalized within the framework of a UPb two-stage evolution. Such a generalization provides an explicit insight into the principle of conventional UPb discordia dating. Its implications for both UPb geochronology and Pb isotopic geology are illustrated for whole-rock
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Four forms of the three-dimensional UPb method established so far are physically generalized within the framework of a UPb two-stage evolution. Such a generalization provides an explicit insight into the principle of conventional UPb discordia dating. Its implications for both UPb geochronology and Pb isotopic geology are illustrated for whole-rock
openaire +1 more source

