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botroids

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- A) Outcrop of the poorly cemented sandstone of the middle member of the Laga fm. containing spheroidal botroids (protruding sandstone concretions), as exposed along the road at the southern foot of Colle Pietro (see Fig. 1 for location); B) The Esinante Creek completely dry as a consequence of the severe drought in the summer of 2022. River banks and bed are virtually made of botroids; C) Exposition at the stone shop selling construction and paving stones from the Laga sandstone, including botroids for garden décor, near the Apiro highway SS76’s exit.
Published: 01 June 2024
Fig. 5 - A) Outcrop of the poorly cemented sandstone of the middle member of the Laga fm. containing spheroidal botroids (protruding sandstone concretions), as exposed along the road at the southern foot of Colle Pietro (see Fig. 1 for location); B) The Esinante Creek completely dry
Image
(a). Field photograph is showing intergrowth of botroids or colloform structures in Sonia sandstone. (b). Field photograph showing botroidal shape or forms vanadium mineralization deposited by epithermal solutions. (c). Field photograph showing vertical movement of mineralizing fluids along faults. (d). Field photograph showing mineralizing vein in between gritty sandstone and pebbly sandstone.
Published: 01 September 2022
Fig.4. (a). Field photograph is showing intergrowth of botroids or colloform structures in Sonia sandstone. (b). Field photograph showing botroidal shape or forms vanadium mineralization deposited by epithermal solutions. (c). Field photograph showing vertical movement of mineralizing
Journal Article
Published: 01 June 2024
Italian Journal of Geosciences (2024) 143 (2): 213–225.
...Fig. 5 - A) Outcrop of the poorly cemented sandstone of the middle member of the Laga fm. containing spheroidal botroids (protruding sandstone concretions), as exposed along the road at the southern foot of Colle Pietro (see Fig. 1 for location); B) The Esinante Creek completely dry...
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Journal Article
Published: 01 March 2014
Jour. Geol. Soc. India (2014) 83 (3): 259–272.
... aggregate comprising cement, veins and botroidal encrustations. Irrespective of its spatial, temporal and paragenetic position, it invariably registers weak to moderate radioactivity, due to the presence of uranium within it, as is evident from microprobe data. Although intra-grain and inter-grain...
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(a–f) SEM and EMP images of elongate and/or skeletal crystals of fayalite (lighter gray) within a glassy matrix (darker gray to black), with white blebs of sulfides (mainly pyrite):(a) modern slag sample showing oxidation of pyrite crystals; (b,c) different fayalite crystal textures of Roman slag samples; (d) fayalite crystals in a matrix of quartz and glass in a Roman slag sample; (e) skeletal fayalite crystals in a modern slag; (f) detail of the previous figure; (g) view of a botroidal growth of iron oxide crystals in a Roman slag; (h) jarosite needle growth within a former sulfide bleb affected by weathering in a modern slag.
Published: 01 October 2009
textures of Roman slag samples; ( d ) fayalite crystals in a matrix of quartz and glass in a Roman slag sample; ( e ) skeletal fayalite crystals in a modern slag; ( f ) detail of the previous figure; ( g ) view of a botroidal growth of iron oxide crystals in a Roman slag; ( h ) jarosite needle growth
Image
(A) Plane polarized light micrograph showing a horizontal, boudinaged sediment layer surrounded by horizontal and vertical celestite veins. Fiber orientations form a continuum between veins I (with a longer fiber displacement history) and II (relatively younger). (B) Plane polarized (above) and crossed polar (below) micrographs of the fibrous celestite fill of a vein. Nested cone-in-cone structures are depicted by minute clay inclusions and crystalline discontinuities. On one hand, their distribution is constrained by fiber shapes; on the other hand, both fibers and cone-in-cone are postdated by botroidal silicifications of quartzine-lutecite. (C) Same as B. Note that cone-in-cone nested discontinuities diverge from sites with clay impurities and that the botroidal silicifications replace the fibrous structure of the vein, which is still recognizable as a ghost feature. (D) Augmented higher-resolution view of the microstructural relationships reported in C. (E) Crossed polar polarized light micrograph showing the two crack sets that delineate cone-in-cone structures and their close relationship with clay impurities. (F) Plane polarized light micrograph showing a celestite-filled and celestite-embedded microfossil containing in its internal cavity crystal discontinuities of the two systems also present outside. These relationships denote the secondary character of cone-in-cone microstructural development with respect to celestite vein precipitation/cementation. (G) Crossed polar polarized light large-magnification micrograph showing the geometrical features associated with the two sets of crystal discontinuities. Set I contains more regular and penetrative discontinuities that correspond to reactivated exfoliation celestite planes. Set II contains more spaced and evident cracks. Likely, they are related to celestite crystallographic planes, too, but at places, these are curved fractures connecting straight crack segments. See text for further details. Note that the vein thin sections shown do not necessarily traverse the geometrical apices of microcones.
Published: 01 March 2011
are postdated by botroidal silicifications of quartzine-lutecite. (C) Same as B. Note that cone-in-cone nested discontinuities diverge from sites with clay impurities and that the botroidal silicifications replace the fibrous structure of the vein, which is still recognizable as a ghost feature. (D) Augmented
Image
Photomicrographs of detrital quartz and feldspar grains in Jeerinah layer at Hesta and Carawine layer at Tarra Tarra turnoff. (A) Quartz grain with undulose extinction from Carawine layer. (B) Randomly distributed fluid inclusions, some with two phases, in quartz grain from Jeerinah layer. (C) Fluid inclusions in quasi-planar arrays in quartz grain from Jeerinah layer. Scale bars in A, B, and C are 20 μm long. (D) Needle-shaped and small fluid inclusions in quartz grain from Carawine layer. Scale bar is 50 μm long. (E) Euhedral feldspar grain between compacted shale intraclasts (to left) and spherule with botroidal rim and irregularly shaped central spot (to right) from Jeerinah layer. Scale bar is 150 μm long. (F) Untwinned feldspar grain with mottled extinction and irregularly distributed inclusions from Jeerinah layer. Thin bright lines in upper middle part of crystal are imperfections in thin section, not mineral inclusions. Scale bar is 120 μm long.
Published: 01 June 2006
intraclasts (to left) and spherule with botroidal rim and irregularly shaped central spot (to right) from Jeerinah layer. Scale bar is 150 μm long. ( F ) Untwinned feldspar grain with mottled extinction and irregularly distributed inclusions from Jeerinah layer. Thin bright lines in upper middle part
Journal Article
Published: 01 September 2022
Jour. Geol. Soc. India (2022) 98 (9): 1199–1204.
...Fig.4. (a). Field photograph is showing intergrowth of botroids or colloform structures in Sonia sandstone. (b). Field photograph showing botroidal shape or forms vanadium mineralization deposited by epithermal solutions. (c). Field photograph showing vertical movement of mineralizing...
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Light microscopy (A–I) and CSLM (J–K) images of the diversity of carbonate microtextures as observed in the Laguna Negra oncoids (for more details see also main text and Table 1). A) Irregular alternation of sparry (s) and wrinkled micritic (m) laminae. B) Transition from irregular sparry (s) and micritic laminae (m) (left) to more regular thinly laminated and predominatly micrite-sparry laminae (right) (ms). C) Translucent sparry laminae composed ofstacked botryoids (sb) alternating with darker micritic to microspar (m) laminae with organic remains including diatom frustules. D, E) Diversity of textures recorded in oncoids and as observed by light microscopy including: micritic (m), sparry (s), diatom-rich granular (g) laminae alternating with filamentous-rich laminae represented by entombed cyanobacteria (Rivularia-like, Riv.) filaments. Note in Parts D and E the subspherical diatom-rich aggregates (some of them highlighted in red, E) that are common in the granular diatom-rich lamina and represent entombed diatom–bacteria aggregates. F) Detail of Rivularia-like filaments encrusted on sparry laminae represented by translucent stacked botroidal crystals (sb). G) Close view of a diatom-rich micritic to microsparitic laminae (Diat) with darker organic remains. H, I) A lamina with oriented pennate diatoms (blue dotted line) alternating with other laminae types (m and s). J, K) CSLM images of laminae underlying the black pustular (Rivularia-like) microbial mat where diatom–bacteria aggregates (highlighted in red) can be observed. Note the abundance of diatoms frustules (Diat.) and photosynthetic pigments highligthed by pigment fluorescence under the confocal microscope.
Published: 19 June 2018
the subspherical diatom-rich aggregates (some of them highlighted in red, E) that are common in the granular diatom-rich lamina and represent entombed diatom–bacteria aggregates. F) Detail of Rivularia -like filaments encrusted on sparry laminae represented by translucent stacked botroidal crystals (sb). G
Journal Article
Journal: GSA Bulletin
Published: 01 March 2011
GSA Bulletin (2011) 123 (3-4): 427–438.
... are postdated by botroidal silicifications of quartzine-lutecite. (C) Same as B. Note that cone-in-cone nested discontinuities diverge from sites with clay impurities and that the botroidal silicifications replace the fibrous structure of the vein, which is still recognizable as a ghost feature. (D) Augmented...
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Journal Article
Journal: Economic Geology
Published: 01 May 2003
Economic Geology (2003) 98 (3): 607–621.
... Botroidal nodules in copper clay matrix 25.08 –10.74 0.38 25 NWX-8 Azurite N15980/W13880; 4,675 177 82 Botroidal nodules in copper clay matrix 24.96 –10.61 0.34 25 NWX-9 Azurite N15200/W14050; 4,900 69 146 From 17-mm-thick azurite vein 23.26 –9.68 0.05 34...
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Journal Article
Published: 08 April 2020
The Canadian Mineralogist (2020) 58 (2): 191–201.
...) with variable quantities of pyrite, sphalerite, chalcopyrite, galena, acanthite, and gold, locally attaining 20% in volume. The main primary textures in the veins are comb, crustiform, and botroidal. The third stage of mineralization occurs as veins (<35 cm thick) and cementing fragments of previous...
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Journal Article
Published: 01 July 2013
Russ. Geol. Geophys. (2013) 54 (7): 653–663.
... traces of the vital activity of marine organisms) is relatively planar or concave, which is best seen in its central zone, where a pebble core, usually with a thin ore crust, is localized. The lower surface is lighter, of botroidal (small-tubercular) texture. The edges have a thin rim of ore substance...
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Journal Article
Published: 01 May 2013
American Mineralogist (2013) 98 (5-6): 977–985.
... Pb 13 13 7 8 18 15 14 * Analyses by XRF. This work was supported by Consejo Nacional de Tecnologia, CONACYT, Project D47075F. High-resolution scanning electron microscopy (HRSEM) of the tuff shows silica glass spherules of ~70 μm diameter with a rough botroidal crustal...
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Journal Article
Published: 01 October 2009
American Mineralogist (2009) 94 (10): 1417–1427.
... textures of Roman slag samples; ( d ) fayalite crystals in a matrix of quartz and glass in a Roman slag sample; ( e ) skeletal fayalite crystals in a modern slag; ( f ) detail of the previous figure; ( g ) view of a botroidal growth of iron oxide crystals in a Roman slag; ( h ) jarosite needle growth...
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Journal Article
Published: 01 September 2018
South African Journal of Geology (2018) 121 (3): 271–286.
... is too fine-grained to identify. The samples often have amygdales with diameters up to 1 mm. The amygdales are commonly filled with clear minerals in the core, probably agate and/or chalcedony and radiating green brown botroidal minerals around the rim, possibly prehnite or zeolites. Major...
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Journal Article
Published: 01 June 2006
South African Journal of Geology (2006) 109 (1-2): 245–261.
... intraclasts (to left) and spherule with botroidal rim and irregularly shaped central spot (to right) from Jeerinah layer. Scale bar is 150 μm long. ( F ) Untwinned feldspar grain with mottled extinction and irregularly distributed inclusions from Jeerinah layer. Thin bright lines in upper middle part...
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Journal Article
Published: 19 June 2018
Journal of Sedimentary Research (2018) 88 (6): 727–742.
... the subspherical diatom-rich aggregates (some of them highlighted in red, E) that are common in the granular diatom-rich lamina and represent entombed diatom–bacteria aggregates. F) Detail of Rivularia -like filaments encrusted on sparry laminae represented by translucent stacked botroidal crystals (sb). G...
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Journal Article
Published: 01 June 2018
Mineralogical Magazine (2018) 82 (3): 491–514.
... Mineralogie Abhandlungen , 148 / 3 , 329 – 336 . Cabral , A.R. , Lehmann , B. , Tupinambà , M. , Schlosser , S. , Kwitko-Ribeiro , R. and Abreu , F.R. ( 2009 ) The platiniferous Au-Pd belt of Minas Gerais, Brazil, and genesis of its botroidal Pt-Pd aggregates . Economic...
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Journal Article
Journal: Economic Geology
Published: 01 September 2024
Economic Geology (2024) 119 (6): 1289–1328.
... ± (Qz, Anh) Mol ± (Cp) None None Chlorite-epidote Very rare Irregular 1–3 Chl, Ep, Act, Cal Py 0.5–2 Ab Calcite Very rare Irregular 1–2 ± (Clays) ± (Py) None None Gray-banded quartz Rare Irregular 2–20 Botroidal Qz ± (Cp, Mol) None None See Table 1 for mineral...
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