نتایج جستجو برای: zircon morphology

تعداد نتایج: 149157  

2016
Hujun Gong Junsheng Nie Zhao Wang Wenbin Peng Rui Zhang Yunxiang Zhang

Single grain zircon U-Pb geochronology has demonstrated great potentials in extracting tectonic and atmospheric circulation signal carried by aeolian, fluvial, and fluviolacustrine sediments. A routine in this sort of studies is analyzing 100-150 grains and then compares zircon U-Pb age spectra between the measured sample and the potential sources. Here we compared the zircon U-Pb age results o...

2012
Balwinder Singh Pradeep Kumar

Abstract — Ceramic shell investment casting process is used to produce high quality metal products with relatively close dimensional tolerances. The refractory primary slurry that is applied to the surface of the pattern assembly, to pick up its surface details plays a very important role in ceramic shell investment casting process (CSICP). It produces a smooth, acceptable surface finish of the...

2016
J. J. Bellucci M. J. Whitehouse A. A. Nemchin J. F. Snape R. T. Pidgeon S. M. Reddy N. Timms

12 Abstract 13 14 The full U-Pb isotopic systematics in a complex lunar zircon ‘Pomegranate’ 15 from lunar impact breccia 73235 have been investigated by the development of a 16 novel Secondary Ion Mass Spectrometry (SIMS) scanning ion imaging (SII) 17 technique. This technique offers at least a four-fold increase in analytical spatial 18 resolution over traditional SIMS analyses in zircon. Res...

Journal: :The Journal of the Geological Society of Japan 1990

2004

Here we report the occurrence, chemistry, and U-Th-Pb isotopic systematics of three meteoritic zircon assemblages, two from the Vaca Muerta mesosiderite and one from the Simmern H5 chondrite. One of the Vaca Muerta zircons occurs in the mesosiderite proper, the other in a eucritic clast associated with chromite, ilmenite, and tridymite, whereas the Simmern zircon occurs in a chondrule composed ...

2008
M. BROWN

Integrated petrographic and chemical analysis of zircon, garnet and rutile from ultrahigh-temperature (UHT) granulites in the Anápolis–Itauçu Complex, Brazil, is used to constrain the significance of zircon ID-TIMS U–Pb geochronological data. Chondrite-normalized rare earth element (REE) profiles of zircon cores have positive-sloping heavy-REE patterns, commonly inferred to be magmatic, whereas...

2015
Thomas Hadlari Graeme T. Swindles Jennifer M. Galloway Kimberley M. Bell Kyle C. Sulphur Larry M. Heaman Luke P. Beranek Karen M. Fallas Axel K Schmitt

Detrital zircon studies are providing new insights on the evolution of sedimentary basins but the role of sedimentary recycling remains largely undefined. In a broad region of northwestern North America, this contribution traces the pathway of detrital zircon sand grains from Proterozoic sandstones through Phanerozoic strata and argues for multi-stage sedimentary recycling over more than a bill...

2005
James M. Mattinson

A long-standing goal in high-precision and high-accuracy U–Pb zircon geochronology is the total elimination of discordance caused by Pb loss. In theory, this is fairly straightforward, but in reality it has proven extremely difficult to attain (or even demonstrate attainment of) this goal. However, a new method, bCA (Chemical Abrasion)-TIMSQ, is capable of completely removing zircon domains tha...

2008
AMANDA L. BOOTH YEHOSHUA KOLODNY C. PAGE CHAMBERLAIN MICHAEL MCWILLIAMS AXEL K. SCHMITT JOSEPH WOODEN

We have investigated U-Pb discordance and oxygen isotopic composition of zircon using high– spatial resolution !O measurement by ion microprobe. !O in both concordant and discordant zircon grains provides an indication of the relationship between fluid interaction and discordance. Our results suggest that three characteristics of zircon are interrelated: (1) U-Pb systematics and concomitant age...

2003
WILLIAM H. PECK JOHN W. VALLEY COLIN M. GRAHAM

Empirical tests of oxygen exchange rate in zircon crystals from amphiboliteand granulite-facies metamorphic rocks of the Grenville Province demonstrate preservation of igneous dO through protracted igneous and metamorphic histories, forming the basis of quantitative estimates of diffusion rate. Granitic orthogneisses, which cooled slowly after granulite-facies metamorphism, show no consistent r...

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