نتایج جستجو برای: zircon morphology

تعداد نتایج: 149157  

2017
Nikola Petricevic Ivan Puhar

A woman (38 years) with tetracycline-stained maxillary anterior teeth came to dental office to improve her appearance. The porcelain veneers and zircon-porcelain crowns were selected as the best treatment option to mask the stained teeth. Medial line, occlusal line, level of gingival margin and frontal plane alignment of maxillary anterior teeth was analysed. Direct composite laminates were pla...

Journal: :Minerals 2022

Singular crypto- and microcrystalline hydrothermal zircon aggregates occur in peralkaline granites from the Corupá Pluton of “A-type” syenites Graciosa Province, Southern Brazil, are herein characterized for their morphological, textural geochemical (major, minor trace elements, Lu-Hf isotopes) properties. The were found to present a variety habits, such as dendritic, oolitic, botryoidal spheru...

Journal: :Anais da Academia Brasileira de Ciencias 2008
Léo A Hartmann Dunyi Liu Yenbin Wang Hans-Joachim Massonne João O S Santos

U-Pb dating of zircon was undertaken with the Beijing SHRIMP II (sensitive high resolution ion microprobe) on anamphibolite facies granodiorite and an almandine-albite granulite from the Santa Maria Chico Granulitic Complex, southern Brazilian Shield. This work was also done to unravel protolith ages which are often hidden in the array of partly reset data. The obtained metamorphic ages of the ...

2016
Nicholas J. Gardiner Christopher L. Kirkland Martin J. Van Kranendonk

Hf isotope ratios measured in igneous zircon are controlled by magmatic source, which may be linked to tectonic setting. Over the 200-500 Myr periodicity of the supercontinent cycle - the principal geological phenomenon controlling prevailing global tectonic style - juvenile Hf signals, i.e. most radiogenic, are typically measured in zircon from granites formed in arc settings (crustal growth),...

Journal: :Anais da Academia Brasileira de Ciencias 2007
Robert S Krymsky Moacir J B Macambira Jean-Michel Lafon Gérson S Estumano

Analytical procedures for U-Pb isotope dilution analyses at the Pará-Iso isotope geology laboratory of the Federal University of Pará (UFPA) are described in detail. The procedures are applied to zircon, titanite, rutile, apatite, columbite-tantalite and whole rock. Reagent preparation and chemical processing are done in clean-room conditions. Samples are dissolved using Teflon microcapsules in...

Journal: :Order 2008
Axel Hultman

A zircon is a poset in which every principal order ideal is finite and equipped with a so-called special matching. We prove that the subposet induced by the fixed points of any automorphism of a zircon is itself a zircon. This provides a natural context in which to view recent results on Bruhat orders on twisted involutions in Coxeter groups. 1. Background and results Let P be a partially order...

2013
Hisatoshi Ito Ryuji Yamada Akihiro Tamura Shoji Arai Kenji Horie Tomokazu Hokada

Although the quest for Earth's oldest rock is of great importance, identifying the youngest exposed pluton on Earth is also of interest. A pluton is a body of intrusive igneous rock that crystallized from slowly cooling magma at depths of several kilometers beneath the surface of the Earth. Therefore, the youngest exposed pluton represents the most recent tectonic uplift and highest exhumation....

Journal: :Proceedings of the National Academy of Sciences of the United States of America 2015
Elizabeth A Bell Patrick Boehnke T Mark Harrison Wendy L Mao

Evidence of life on Earth is manifestly preserved in the rock record. However, the microfossil record only extends to ∼ 3.5 billion years (Ga), the chemofossil record arguably to ∼ 3.8 Ga, and the rock record to 4.0 Ga. Detrital zircons from Jack Hills, Western Australia range in age up to nearly 4.4 Ga. From a population of over 10,000 Jack Hills zircons, we identified one >3.8-Ga zircon that ...

2013
Christoph Lenz Dominik Talla Katja Ruschel Radek Škoda Jens Götze Lutz Nasdala

In this paper, possibilities and limits of the application of REE3+ luminescence (especially the Nd3+4F3/2 → 4I9/2 emission) as structural probe are evaluated. Important factors controlling the Nd3+ luminescence signal are discussed, including effects of the crystal-field, crystal orientation, structural state, and temperature. Particular attention was paid to the study of the accessory mineral...

نمودار تعداد نتایج جستجو در هر سال

با کلیک روی نمودار نتایج را به سال انتشار فیلتر کنید