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clinojimthompsonite

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Journal Article
Published: 01 December 1978
American Mineralogist (1978) 63 (11-12): 1053–1073.
...D. R. Veblen; C. W. Burnham Abstract The crystal structures of jimthompsonite, clinojimthompsonite, and chesterite have been solved and refined using three-dimensional X-ray intensity data. Jimthompsonite and clinojimthompsonite contain I-beams composed of triple silicate chains and wide octahedral...
Image
The I-beam of <span class="search-highlight">clinojimthompsonite</span> projected on to (100) and showing tetrahe...
Published: 01 December 2009
F ig . 23. The I-beam of clinojimthompsonite projected on to (100) and showing tetrahedra T (1,2,3), the ribbon of octahedra and the three distinct potential sites for molecular H 2 O W (1,2,3). The water sites lie in the channel in a plane parallel to (100) and are 3 Å apart. There is one
Journal Article
Published: 01 December 1981
American Mineralogist (1981) 66 (11-12): 1107–1134.
... reactions include amphibole, clinojimthompsonite, chain-width disordered pyribole, and several sheet silicates. Textural considerations indicate that there are a number of different paths for pyroxene hydration reactions. These include the simple paths pyroxene → amphibole, pyroxene → clinojimthompsonite...
Image
( a  and  b ) Atom filling models for crystal structures of ferro-tschermak...
Published: 01 April 2022
Figure 1. ( a and b ) Atom filling models for crystal structures of ferro-tschermakite and clinojimthompsonite projected onto [001] showing occupancy of cation sites as marked. Crystallographic information data from Hawthorne and Grundy (1973) and Veblen and Burnham (1978) . The two building
Journal Article
Published: 01 May 2011
American Mineralogist (2011) 96 (5-6): 814–819.
... clinojimthompsonite (Na-cjt) with existing data for various common minerals (i.e., enstatite, talc, anthophyllite, and chrysotile). We also present new experimental data to show that Na-cjt should form stably at typical metamorphic conditions of 0.2 GPa and 450 °C. Ion-activity vs. pH diagrams calculated at 100–300...
FIGURES
Journal Article
Published: 01 October 2024
American Mineralogist (2024) 109 (10): 1798–1818.
... to triple I beam zippers, including pyroxene slabs, to longer NCP polysomes up to 15-I beam chains. Clinojimthompsonite (Cjim) is observed for the first time within magnetite. Although no discrete polysomes could be defined, the NCP-amphibole intergrowths have compositions between Mg-Fe amphiboles and Cjim...
FIGURES | View All (15)
Journal Article
Published: 01 October 1978
American Mineralogist (1978) 63 (9-10): 1000–1009.
.... The cell parameters of the minerals are diagnostic: (1) jimthompsonite is orthorhombic, Pbca, a = 18.6, b = 27.2, с = 5.30A; (2) clinojimthompsonite is monoclinic, C 2/ c, a = 9.87, b = 27.2, с = 5.32A, β = 109.5°; (3) chesterite is orthorhombic, A 2 1 ma, a = 18.6, b = 45.3, с = 5.30A; (4) an unnamed...
Image
( a  and  b ) Wider, more regular blocks triple chain slabs (up to 23; in b...
Published: 01 October 2024
Figure 10. ( a and b ) Wider, more regular blocks triple chain slabs (up to 23; in blue) within amphibole (gray ribbon underneath). Sequence in b represent a full transect of clinojimthompsonite (Cjim) (grain in Fig. 3a ) shown as high-resolution images in c–f . FFT pattern as inset to c
Journal Article
Published: 01 April 2022
American Mineralogist (2022) 107 (4): 765–777.
...Figure 1. ( a and b ) Atom filling models for crystal structures of ferro-tschermakite and clinojimthompsonite projected onto [001] showing occupancy of cation sites as marked. Crystallographic information data from Hawthorne and Grundy (1973) and Veblen and Burnham (1978) . The two building...
FIGURES | View All (10)
Journal Article
Published: 01 February 2008
American Mineralogist (2008) 93 (2-3): 351–359.
..., and were named jimthompsonite [Mg 10 Si 12 O 32 (OH) 4 ; Pbca ] and chesterite [Mg 17 Si 20 O 54 (OH) 6 ; A 2 1 ma ] ( Veblen and Burnham 1978a , 1978b ; Veblen et al. 1977 ). Their monoclinic polymorphs are, respectively, clinojimthompsonite ( C 2/ c ) and an unnamed mineral ( A 2/ m ) (e.g., Droop...
FIGURES | View All (9)
Journal Article
Published: 01 December 2009
Mineralogical Magazine (2009) 73 (6): 957–996.
...F ig . 23. The I-beam of clinojimthompsonite projected on to (100) and showing tetrahedra T (1,2,3), the ribbon of octahedra and the three distinct potential sites for molecular H 2 O W (1,2,3). The water sites lie in the channel in a plane parallel to (100) and are 3 Å apart. There is one...
FIGURES | View All (24)
Journal Article
Published: 01 August 2009
American Mineralogist (2009) 94 (8-9): 1242–1254.
... silicates have not yet been synthesized, this study focused on the Na-analogue to clinojimthompsonite (Na-cjt), which forms readily in a laboratory setting. Synthetic Na-cjt was characterized using electron microscopy and microanalysis, thermogravimetric analysis, infrared spectroscopy, and loss on ignition...
FIGURES | View All (12)
Journal Article
Published: 01 May 2007
American Mineralogist (2007) 92 (5-6): 898–908.
... experiment, a calcian clinojimthompsonite domain extending 15 unit cells along the b axis was observed. The sample after 582 h and five retreatments shows, on average, 3.5% true solid solution with Mg expressed as the Mg-cummingtonite (MC) component after correction for the presence of CMFs. This sample...
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Journal Article
Published: 01 October 1994
American Mineralogist (1994) 79 (9-10): 909–920.
... amphibole of grunerite composition containing no detectable amount of Cl but intergrown with submicrometer-sized slabs of Cl-rich annite (2.8 wt%), Fe-rich talc, Fe-rich clinojimthompsonite, and very wide chain silicate. TEM-AEM study of prograde hastingsite and biotite suggests that Cl is dissolved...
Journal Article
Published: 01 June 1991
American Mineralogist (1991) 76 (5-6): 728–732.
...) with composition near that of talc, (Mg,Fe) 3 Si 4 O 10 (OH) 2 . The calculations were performed using results of the structure refinements of two orthopyroxenes (Opx), clinoenstatite (Cpx), twoampiboles (anthophyllite = An, cummingtonite = Cu), chesterite (Ch), jimthompsonite (Jt), clinojimthompsonite, and talc...
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Low-resolution images illustrating amphibole-NCP intergrowths from ( a ) ro...
Published: 01 October 2024
Figure 3. Low-resolution images illustrating amphibole-NCP intergrowths from ( a ) rounded, and ( b ) subhedral grains, and ( c–g ) aggregates (areas marked on Fig. 2 ). Crystal of clinojimthompsonite with amphibole intergrowths (lighter bands) in a . Note changes in chemical composition along
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Structures of amphibole (left) and TCS (right). The amphibole structure is ...
Published: 01 December 2009
F ig . 1. Structures of amphibole (left) and TCS (right). The amphibole structure is that of `magnesiorichterite' (MR), P 2 1 / m ( Cámara et al ., 2003 ); the TCS structure is that of clinojimthompsonite, C 2/ c ( Veblen and Burnham, 1978 ). The synthetic TCSs described in this paper have
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In the polysomatic model of  Thompson (1970 ,  1978 ,  1981 ), amphibole ca...
Published: 01 October 2007
the triple-chain clinojimthompsonite structure built from mica and pyroxene modules in a 2:1 ratio. Allowing disordered sequences of mica and pyroxene building blocks can result in many different possible structure types. View parallel to the silicate chains. From Veblen (1981) .
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HAADF STEM simulations ( a  and  b ) and images ( c  and  d ) showing relat...
Published: 01 April 2022
Figure 9. HAADF STEM simulations ( a and b ) and images ( c and d ) showing relationships between I-beam models (digits corresponding to the number of chains) and unit cells of ferro-tschermakite and clinojimthompsonite projected/imaged on [001] zone axis. ( a and b ) Two rows of I-beam
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Models and images of chain silicates as labeled, each plotted on [001] zone...
Published: 01 October 2024
Figure 6. Models and images of chain silicates as labeled, each plotted on [001] zone axis. The structures used for the three models at the top are: actinolite for amphibole ( Evans and Yang 1998 ), clinojimthompsonite for triple-chain silicate, and chesterite for the alternating double