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dypingite

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Journal Article
Published: 07 May 2025
American Mineralogist (2025)
...Yang Lu; Anton Sednev-Lugovets; Patricia Carvalho; Matylda N. Guzik; Amir Masoud Dayaghi; Kristina Dunkel; Håkon Austrheim; Zhiyong Lin; Henrik Friis Abstract Dypingite has recently been found to have promising applications in material and environmental sciences. However, its exploitation...
Journal Article
Published: 01 November 2006
Proceedings of the Yorkshire Geological Society (2006) 56 (2): 151–154.
...D. I. Green; B. Young SUMMARY The rare basic hydrated magnesium carbonate minerals hydromagnesite and dypingite are reported from low temperature hydrothermal Pb–Zn deposits in the Alston Block of the Northern Pennine Orefield. Both minerals occur as very late stage constituents of deposits rich...
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Journal Article
Published: 01 October 1970
American Mineralogist (1970) 55 (9-10): 1457–1465.
...Gunnar Raade Abstract The new mineral dypingite was found in the Dypingdal serpentine-magnesite deposit, Snarum, South Norway, where it occurs as a thin cover on serpentine. It is of late secondary origin, deposited from cold, leaching solutions. Chemical analysis of 100 mg of handpicked material...
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Modes in which hydrated magnesium carbonate minerals have been identified at Clinton Creek, Yukon Territory and Cassiar, British Columbia: (A) nesquehonite/dypingite crust from Cassiar, (B) dypingite on cobble from Clinton Creek, (C) nesquehonite/dypingite/hydromagnesite spires from Clinton Creek, and (D) disseminated cement of hydromagnesite from Clinton Creek.
Published: 01 August 2006
F igure 2. Modes in which hydrated magnesium carbonate minerals have been identified at Clinton Creek, Yukon Territory and Cassiar, British Columbia: ( A ) nesquehonite/dypingite crust from Cassiar, ( B ) dypingite on cobble from Clinton Creek, ( C ) nesquehonite/dypingite/hydromagnesite spires
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Phase diagram for MHC, calcite, aragonite, and dypingite precipitation at 23 °C as a function of Mg concentration in solution and (a) initial pH, (b) final pH. Note solid fill = fields from initial pH, dashed fill = extended fields from final pH. (Color online.)
Published: 01 August 2021
Figure 8. Phase diagram for MHC, calcite, aragonite, and dypingite precipitation at 23 °C as a function of Mg concentration in solution and ( a ) initial pH, ( b ) final pH. Note solid fill = fields from initial pH, dashed fill = extended fields from final pH. (Color online.)
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FT-IR spectrum of the 60°C surface film. The infrared spectra of dypingite and hydromagnesite are extensively similar (Raade 1970; White 1974). Absorption bands resulting from  OH- groups ( 3650 cm–1) and water of crystallization (3510 and  3450 cm–1) are identical for both, as are CO32- stretching bands (1480, 1420, and  1120 cm–1) and CO32- bending bands (880 and  850 cm–1).
Published: 01 July 2008
Figure 7.  FT-IR spectrum of the 60°C surface film. The infrared spectra of dypingite and hydromagnesite are extensively similar (Raade 1970 ; White 1974 ). Absorption bands resulting from OH - groups ( 3650 cm –1 ) and water of crystallization (3510 and 3450 cm –1 ) are identical
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Backscattered electron (BSE) images of horizontal crust sample 04CC0702 (A), (C), and (D) and vertical crust sample 04CC0201B (B). (A). Nesquehonite at the surface of sample 04CC0702 with dypingite + hydromagnesite nucleating on serpentine. (B). Rosettes of dypingite nucleating on grains of serpentine at depth in sample 04CC0201B. (C). Nesquehonite infilling dissolution fissures in a grain of serpentine near the surface of crust sample 04CC0702. (D). Nesquehonite filling cracks in a fractured grain of serpentine. D = dypingite, H = hydromagnesite, M = magnetite, N = nesquehonite, S = serpentine.
Published: 01 January 2009
F ig . 5. Backscattered electron (BSE) images of horizontal crust sample 04CC0702 (A), (C), and (D) and vertical crust sample 04CC0201B (B). (A). Nesquehonite at the surface of sample 04CC0702 with dypingite + hydromagnesite nucleating on serpentine. (B). Rosettes of dypingite nucleating
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Summary diagram of mechanisms of formation for three modes of occurrence of secondary carbonate minerals: (A) nesquehonite-rich efflorescences on vertical and horizontal surfaces, (B) grains of serpentine cemented by dypingite ± hydromagnesite below the surface of the tailings pile, and (C) coatings of dypingite ± hydromagnesite on grains of serpentine. Details of mineral occurrences are illustrated in the corresponding boxes. Small grains of serpentine are not shown in the main figure for simplicity but are included in boxes A, B, and C.
Published: 01 January 2009
F ig . 6. Summary diagram of mechanisms of formation for three modes of occurrence of secondary carbonate minerals: (A) nesquehonite-rich efflorescences on vertical and horizontal surfaces, (B) grains of serpentine cemented by dypingite ± hydromagnesite below the surface of the tailings pile
Journal Article
Published: 01 August 2021
American Mineralogist (2021) 106 (8): 1294–1305.
...Figure 8. Phase diagram for MHC, calcite, aragonite, and dypingite precipitation at 23 °C as a function of Mg concentration in solution and ( a ) initial pH, ( b ) final pH. Note solid fill = fields from initial pH, dashed fill = extended fields from final pH. (Color online.) ...
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Journal Article
Journal: Economic Geology
Published: 01 January 2009
Economic Geology (2009) 104 (1): 95–112.
...F ig . 5. Backscattered electron (BSE) images of horizontal crust sample 04CC0702 (A), (C), and (D) and vertical crust sample 04CC0201B (B). (A). Nesquehonite at the surface of sample 04CC0702 with dypingite + hydromagnesite nucleating on serpentine. (B). Rosettes of dypingite nucleating...
FIGURES | View All (9)
Journal Article
Published: 01 July 2008
The Journal of Geology (2008) 116 (4): 387–400.
...Figure 7.  FT-IR spectrum of the 60°C surface film. The infrared spectra of dypingite and hydromagnesite are extensively similar (Raade 1970 ; White 1974 ). Absorption bands resulting from OH - groups ( 3650 cm –1 ) and water of crystallization (3510 and 3450 cm –1 ) are identical...
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SEM images of the precipitates from Spring #1 (a,b) and Spring #2 (c,d). (a) The carbonate surface film from Fig. 1a, sample OM01: rhombohedral calcite in a network of aragonite needles. (b) Sample OM03, dypingite rosettes (black arrow) surrounded by acicular aragonite; (c) Sample OM08 from Fig. 1b, crystals of aragonite; (d) close-up of the same area showing a secondary phase (black arrows) growing from or nucleating on the aragonite crystals. These crystals are probably dypingite. Samples OM03 and OM08 were collected from the bottom of the springs.
Published: 01 November 2014
F ig . 4. SEM images of the precipitates from Spring #1 ( a,b ) and Spring #2 ( c,d ). ( a ) The carbonate surface film from Fig. 1 a , sample OM01: rhombohedral calcite in a network of aragonite needles. ( b ) Sample OM03, dypingite rosettes (black arrow) surrounded by acicular aragonite; ( c
Journal Article
Published: 01 April 2024
Mineralogical Magazine (2024) 88 (2): 162–169.
...) hydromagnesite/dypingite formed at 60°C; (e) back-scattered electron and LA-ICP-MS maps showing the distribution of Mg and Cr nesquehonite prismatic crystals; (f) back-scattered electron and LA-ICP-MS maps showing the distribution of Mg and Cr in the hydromagnesite, 20°C; (g) LA-ICP-MS maps showing...
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Representative EDX spectra: (a) calcite (No. 14; Table 2), (b) aragonite (No. 25; Table 2), (c) dypingite (No. 29; Table 2).
Published: 01 August 2021
Figure 7. Representative EDX spectra: ( a ) calcite (No. 14; Table 2 ), ( b ) aragonite (No. 25; Table 2 ), ( c ) dypingite (No. 29; Table 2 ).
Journal Article
Published: 01 August 2006
American Mineralogist (2006) 91 (8-9): 1331–1341.
...F igure 2. Modes in which hydrated magnesium carbonate minerals have been identified at Clinton Creek, Yukon Territory and Cassiar, British Columbia: ( A ) nesquehonite/dypingite crust from Cassiar, ( B ) dypingite on cobble from Clinton Creek, ( C ) nesquehonite/dypingite/hydromagnesite spires...
FIGURES | View All (8)
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Representative Raman spectra: (a) calcite (No. 6; Table 2); (b) aragonite (No. 11; Table 2); (c) MHC (No. 9; Table 2); (d) dypingite (No. 16; Table 2).
Published: 01 August 2021
Figure 3. Representative Raman spectra: ( a ) calcite (No. 6; Table 2 ); ( b ) aragonite (No. 11; Table 2 ); ( c ) MHC (No. 9; Table 2 ); ( d ) dypingite (No. 16; Table 2 ).
Journal Article
Published: 01 November 2014
Mineralogical Magazine (2014) 78 (6): 1479–1490.
...F ig . 4. SEM images of the precipitates from Spring #1 ( a,b ) and Spring #2 ( c,d ). ( a ) The carbonate surface film from Fig. 1 a , sample OM01: rhombohedral calcite in a network of aragonite needles. ( b ) Sample OM03, dypingite rosettes (black arrow) surrounded by acicular aragonite; ( c...
FIGURES | View All (5)
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SEM images of MHC: (a) connected spheres (No. 15; Table 2), (b) aragonite overgrowth (bright) on MHC sphere (No. 21; Table 2), (c) aragonite (bright) and dypingite (dark) overgrowth on MHC sphere (No. 32; Table 2), (d) surface of MHC sphere (No. 31; Table 2).
Published: 01 August 2021
Figure 6. SEM images of MHC: ( a ) connected spheres (No. 15; Table 2 ), ( b ) aragonite overgrowth (bright) on MHC sphere (No. 21; Table 2 ), ( c ) aragonite (bright) and dypingite (dark) overgrowth on MHC sphere (No. 32; Table 2 ), ( d ) surface of MHC sphere (No. 31; Table 2 ).
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Representative scanning electron micrographs of (A) nesquehonite, (B) dypingite, (C) hydromagnesite, and (D) magnesite collected from hydromagnesite–magnesite playas near Atlin, British Columbia, Canada. These minerals are potential products in carbon mineralization processes. Micrographs by Ian Power.
Published: 01 January 2013
Figure 5 Representative scanning electron micrographs of (A) nesquehonite, (B) dypingite, (C) hydromagnesite, and (D) magnesite collected from hydromagnesite–magnesite playas near Atlin, British Columbia, Canada. These minerals are potential products in carbon mineralization processes
Journal Article
Journal: Elements
Published: 01 February 2023
Elements (2023) 19 (1): 22–29.
... of soluble amorphous phases may control (Ca–)Mg-carbonate formation (e.g., Zeyen et al. 2021 ; Raudsepp et al. 2022 ). Figure 2. ( A–C ) Scanning electron microscopy images and ( D–E ) photographs of carbonates from various alkaline lakes. ( A ) Nesquehonite (Nes) and ( B ) dypingite (Dyp) from...
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