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coprecipitation

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Journal Article
Journal: Geology
Published: 09 July 2024
Geology (2024) 52 (10): 737–741.
... coprecipitation of Au and amorphous silica and subsequent recrystallization to test whether this is a viable mechanism to generate Au nuggets within quartz veins. Within minutes, coprecipitation of amorphous silica and Au nanoparticles occurred, representing an effective Au deposition mechanism. Within one week...
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Journal Article
Published: 01 December 2017
American Mineralogist (2017) 102 (12): 2512–2520.
...Xu Ma; Zidan Yuan; Mario A. Gomez; Xin Wang; Shaofeng Wang; Shuhua Yao; Yongfeng Jia Abstract Arsenic (As), barium (Ba), and sulfate (SO 4 2– ), coexisting in natural and mining impacted environments, possibly lead to As-barite coprecipitation. This work investigated the coprecipitation of Ba 2...
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Journal Article
Published: 01 June 2016
Clays and Clay Minerals (2016) 64 (3): 283–298.
... ≈ 0.15 in the structure of these goethites. Why the cell parameters did not vary as observed for Al-goethites prepared by conventional coprecipitation methods remains unclear, however. The loss of mass occurring at ~750°C, which is associated with the decomposition of sulfate ( Leetma et al ., 2014...
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Journal Article
Published: 01 February 2006
Clays and Clay Minerals (2006) 54 (1): 45–53.
...) and chemically homologous Eu(III) coprecipitated with Mg(OH) 2 as a precursor. X-ray diffraction, Fourier transform infrared spectroscopy and atomic force microscopy identified the reaction products unambiguously as hectorite. The sorption mechanisms of Eu associated with the synthesized hectorite were...
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Journal Article
Journal: Economic Geology
Published: 01 July 1992
Economic Geology (1992) 87 (4): 1191–1192.
Journal Article
Journal: Economic Geology
Published: 01 July 1992
Economic Geology (1992) 87 (4): 1192–1193.
Journal Article
Journal: Economic Geology
Published: 01 August 1991
Economic Geology (1991) 86 (5): 1070–1082.
...) coprecipitation of sphalerite and chalcopyrite is an alternative mechanism of formation of the chalcopyrite inclusions in the ore deposits studied. GeoRef, Copyright 2006, American Geological Institute. Abstract, Copyright, Society of Economic Geologists 1991 ...
Journal Article
Published: 01 August 1990
American Mineralogist (1990) 75 (7-8): 840–846.
.... A detailed examination shows that the small platelet-shaped crystals of magnetite occur only inside or along the amphibole lamellae. The phases are inferred to have coprecipitated, governed by the diffusion of H into the sample (diopside 1 + H 2 → diopside 2 + amphibole + magnetite). Such a reaction implies...
Journal Article
Published: 01 February 1989
Clays and Clay Minerals (1989) 37 (1): 12–18.
Journal Article
Published: 01 September 1987
Journal of Sedimentary Research (1987) 57 (5): 928–937.
Journal Article
Journal: Economic Geology
Published: 01 December 1984
Economic Geology (1984) 79 (8): 1951–1952.
Journal Article
Journal: Economic Geology
Published: 01 December 1984
Economic Geology (1984) 79 (8): 1953–1955.
Journal Article
Journal: Economic Geology
Published: 01 October 1983
Economic Geology (1983) 78 (6): 1144–1203.
Journal Article
Journal: AAPG Bulletin
Published: 01 March 1972
AAPG Bulletin (1972) 56 (3): 622–623.
Journal Article
Journal: Clay Minerals
Published: 01 June 1987
Clay Minerals (1987) 22 (2): 207–223.
Journal Article
Journal: Clay Minerals
Published: 01 December 1986
Clay Minerals (1986) 21 (5): 861–877.
Image
Petrography. A–C. Nori/RA prospect. (A) Biotite (bio)-K-feldspar (ksp)-quartz-magnetite (mag) (Nomag1) metasiltstone. Nomag1 occurs as fine grains randomly disseminated in the metasiltstone. (B) Magnetite (Nomag2) coprecipitated with tourmaline (tur)-biotite (bt)-uraninite (ur)-molybdenite (mol) in veins. (C) Nomag2 coprecipitated with pyrite (py) in ore veins. D–G. NICO deposit. (D) Fine-grained pre-ore magnetite (NImag1) disseminated along the bedding. NImag1 has multiple silicate inclusions as it overgrows and replaces silicates. (E) Coarse-grained NImag2 coprecipitated with arsenopyrite (apy). Late bismuthinite (bm) is intergranular to both. (F) Magnetite (NImag3) and bismuthinite (bm), intergranular and filling fractures in arsenopyrite. (G) Coarse-grained magnetite from the Terra magnetite-apatite (ap) body coprecipitated with apatite. (H) Damp prospect. Chalcopyrite crosscutting coarse grains of pyrite and magnetite. I–J. Sue-Dianne deposit. (I) Magnetite and carrollite (car) coprecipitated; late chalcopyrite intergranular to both. Hematite is altering magnetite. (J) Epidote and magnetite coprecipitated and late chalcopyrite and emplectite (emp) are intergranular to them. Locally, hematite alters magnetite. K–L. Fab prospect. (K) Fine-grained magnetite (Fmag1) with silicate inclusions (incl). (L) Magnetite (Fmag2) occurring in a vein coprecipitated with pyrite.
Published: 01 November 2014
Fig. 8 Petrography. A–C. Nori/RA prospect. (A) Biotite (bio)-K-feldspar (ksp)-quartz-magnetite (mag) (Nomag1) metasiltstone. Nomag1 occurs as fine grains randomly disseminated in the metasiltstone. (B) Magnetite (Nomag2) coprecipitated with tourmaline (tur)-biotite (bt)-uraninite (ur)-molybdenite
Image
U LIII-edge XANES spectra; (a) uraninite (U(IV) reference); (b) OCL adsorption; (c) YCL adsorption; (d) OCL coprecipitation reduced; (e) OCL coprecipitation oxidized; (f) YCL coprecipitation reduced; (g) schoepite (U(VI) reference).
Published: 01 November 2015
F ig . 3. U L III -edge XANES spectra; ( a ) uraninite (U(IV) reference); ( b ) OCL adsorption; ( c ) YCL adsorption; ( d ) OCL coprecipitation reduced; ( e ) OCL coprecipitation oxidized; ( f ) YCL coprecipitation reduced; ( g ) schoepite (U(VI) reference).
Image
U LIII-edge k3-weighted EXAFS spectra (left) and Fourier transforms plotted without a phase shift (right). Black lines are data and red lines are fits to the data; (a) OCL adsorption; (b) OCL coprecipitation reduced; (c) OCL coprecipitation oxidized; (d) YCL coprecipitation reduced.
Published: 01 November 2015
F ig . 4. U L III -edge k3-weighted EXAFS spectra (left) and Fourier transforms plotted without a phase shift (right). Black lines are data and red lines are fits to the data; ( a ) OCL adsorption; ( b ) OCL coprecipitation reduced; ( c ) OCL coprecipitation oxidized; ( d ) YCL coprecipitation
Image
Backscattered electron (BSE) image (A) showing coprecipitated barite and ferroselite in a grain separate from MU10-10801C 384.5’. Selenium-bearing pyrite is also present along the right-hand perimeter of the grain, which precipitated prior to ferroselite and barite. The BSE image is accompanied with element maps of barium (B, red), iron (C, blue), sulfur (D, yellow), and selenium (E, green).
Published: 01 March 2019
Fig. 16. Backscattered electron (BSE) image (A) showing coprecipitated barite and ferroselite in a grain separate from MU10-10801C 384.5’. Selenium-bearing pyrite is also present along the right-hand perimeter of the grain, which precipitated prior to ferroselite and barite. The BSE image