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Journal Article

Chattermark Trails: Surface Features on Detrital Quartz Grains Indicative of a Tropical Climate Available to Purchase

Katharina M. Peterknecht, Gerd F. Tietz
Published: 01 February 2011
Journal of Sedimentary Research (2011) 81 (2): 153–158.
DOI: https://doi.org/10.2110/jsr.2011.9
... are chattermark trails. Chattermark trails are a series of linearly arranged, rune-like grooves on surfaces of minerals grains, such as quartz and garnet, lacking any type of cleavage. These trails have been described from many unconsolidated sediments and are attributed mostly to glacial sediments. Laboratory...
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View PDF for article title, <span class="search-highlight">Chattermark</span> <span class="search-highlight">Trails</span>: Surface Features on Detrital Quartz Grains Indicative of a Tropical Climate
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Journal Article

Chattermark trails as paleoenvironmental indicators Available to Purchase

Peter A. Bull, Stephen J. Culver, Rita Gardner
Journal: Geology
Published: 01 July 1980
Geology (1980) 8 (7): 318–322.
DOI: https://doi.org/10.1130/0091-7613(1980)8<318:CTAPI>2.0.CO;2
... similar features. Considerable caution is advised when using these chattermark trails as one-step indicators of glaciation. Geological Society of America 1980 ...
View PDF for article title, <span class="search-highlight">Chattermark</span> <span class="search-highlight">trails</span> as paleoenvironmental indicators
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Journal Article

Glacial deposits identified by chattermark trails in detrital garnets: Comment and reply: REPLY Available to Purchase

Robert L. Folk
Journal: Geology
Published: 01 January 1978
Geology (1978) 6 (1): 10.
DOI: https://doi.org/10.1130/0091-7613(1978)6<10a:GDIBCT>2.0.CO;2
View PDF for article title, Glacial deposits identified by <span class="search-highlight">chattermark</span> <span class="search-highlight">trails</span> in detrital garnets: Comment and reply: REPLY
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Journal Article

Chattermark trails on heavy minerals in glacial sediments Available to Purchase

C. P. Gravenor, T. A. McIelwain, M. Stupavsky
Journal: Geology
Published: 01 January 1978
Geology (1978) 6 (1): 61–63.
DOI: https://doi.org/10.1130/0091-7613(1978)6<61:CTOHMI>2.0.CO;2
View PDF for article title, <span class="search-highlight">Chattermark</span> <span class="search-highlight">trails</span> on heavy minerals in glacial sediments
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Journal Article

Glacial deposits identified by chattermark trails in detrital garnets: Comment and reply Available to Purchase

A. C. Rocha-Campos, E. B. Krauspenhar
Journal: Geology
Published: 01 January 1978
Geology (1978) 6 (1): 8–9.
DOI: https://doi.org/10.1130/0091-7613(1978)6<8:GDIBCT>2.0.CO;2
View PDF for article title, Glacial deposits identified by <span class="search-highlight">chattermark</span> <span class="search-highlight">trails</span> in detrital garnets: Comment and reply
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Journal Article

Glacial deposits identified by chattermark trails in detrital garnets: Comment and reply: COMMENT Available to Purchase

Peter A. Bull
Journal: Geology
Published: 01 April 1977
Geology (1977) 5 (4): 248.
DOI: https://doi.org/10.1130/0091-7613(1977)5<248:GDIBCT>2.0.CO;2
View PDF for article title, Glacial deposits identified by <span class="search-highlight">chattermark</span> <span class="search-highlight">trails</span> in detrital garnets: Comment and reply: COMMENT
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Journal Article

Glacial deposits identified by chattermark trails in detrital garnets: Comment and reply: REPLY Available to Purchase

Robert L. Folk
Journal: Geology
Published: 01 April 1977
Geology (1977) 5 (4): 249.
DOI: https://doi.org/10.1130/0091-7613(1977)5<249a:GDIBCT>2.0.CO;2
View PDF for article title, Glacial deposits identified by <span class="search-highlight">chattermark</span> <span class="search-highlight">trails</span> in detrital garnets: Comment and reply: REPLY
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Journal Article

Glacial deposits identified by chattermark trails in detrital garnets Available to Purchase

Robert L. Folk
Journal: Geology
Published: 01 August 1975
Geology (1975) 3 (8): 473–475.
DOI: https://doi.org/10.1130/0091-7613(1975)3<473:GDIBCT>2.0.CO;2
View PDF for article title, Glacial deposits identified by <span class="search-highlight">chattermark</span> <span class="search-highlight">trails</span> in detrital garnets
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Journal Article

New scents on the chattermark trail; weathering enhances obscure microfractures Available to Purchase

Elizabeth Decker Orr, Robert L. Folk
Published: 01 March 1983
Journal of Sedimentary Research (1983) 53 (1): 121–129.
DOI: https://doi.org/10.1306/212F8166-2B24-11D7-8648000102C1865D
...Elizabeth Decker Orr; Robert L. Folk Abstract The occurrence of chattermark trails varies with weathering on glacial garnet sand grains but not on quartz grains. More garnet grains in contact with humic acids near a soil zone are chattermarked and more chattermark trails occur per grain. Artificial...
View PDF for article title, New scents on the <span class="search-highlight">chattermark</span> <span class="search-highlight">trail</span>; weathering enhances obscure microfractures
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Image
SEM images of additional scratches and chattermark trails on the etched surface of another quartz bead. The scratches are straight, and the grooves of the chattermark trails are straight or curved.

SEM images of additional scratches and chattermark trails on the etched sur... Available to Purchase

Published: 01 February 2011
Figure 4 SEM images of additional scratches and chattermark trails on the etched surface of another quartz bead. The scratches are straight, and the grooves of the chattermark trails are straight or curved.
Journal Article

Chattermarked garnets in Pleistocene glacial sediments Available to Purchase

C. P. GRAVENOR
Journal: GSA Bulletin
Published: 01 August 1982
GSA Bulletin (1982) 93 (8): 751–758.
DOI: https://doi.org/10.1130/0016-7606(1982)93<751:CGIPGS>2.0.CO;2
...C. P. GRAVENOR Abstract An examination of the surface textures on detrital garnets shows that conchoidal fractures, V-shaped etch pits, and other marks of unknown origin can be modified by chemical etching to produce features which resemble chattermark trails produced by slip-stick motion. In order...
View PDF for article title, <span class="search-highlight">Chattermarked</span> garnets in Pleistocene glacial sediments
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Journal Article

The nature of the Late Paleozoic glaciation in Gondwana as determined from an analysis of garnets and other heavy minerals Free

C. P. Gravenor
Published: 01 June 1979
Canadian Journal of Earth Sciences (1979) 16 (6): 1137–1153.
DOI: https://doi.org/10.1139/e79-101
... environments during periods of deglaciation.An analysis of chattermark trails found on the surface of the garnets shows that the percentage of chattermarked garnets is roughly twice that from samples of Pleistocene glacial sediments of North America. As the percentage of garnets with chattermark trails...
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Journal Article

Chattermarked garnets and heavy minerals from the Late Paleozoic glacial deposits of southeastern Brazil Free

C. P. Gravenor
Published: 01 January 1980
Canadian Journal of Earth Sciences (1980) 17 (1): 156–159.
DOI: https://doi.org/10.1139/e80-013
...C. P. Gravenor Abstract Heavy mineral suites from Late Paleozoic tillites from the southeastern part of the Paraná Basin are dominated by garnet. An analysis of the heavy minerals and chattermark trails found on the garnets suggests that the glacial sediments were transported over long distances...
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Journal Article

Heavy minerals and sedimentological studies on the glaciogenic Late Precambrian Gaskiers Formation of Newfoundland Free

C. P. Gravenor
Published: 01 October 1980
Canadian Journal of Earth Sciences (1980) 17 (10): 1331–1341.
DOI: https://doi.org/10.1139/e80-140
... and rutile. The garnets are angular, fresh in appearance, and about 9% of the garnets have glacially derived chattermark trails. This observation, along with the presence of striated and facetted clasts, suggest that at some time prior to final deposition, the diamictites underwent transport in glaciers...
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Image
SEM image of detrital quartz grain from beach sediment (Vår Haller, Sweden, grain size = 520 μm). This quartz grain was also etched with dilute hydrofluoric acid (10%) for 25 minutes. It shows a high abundance of interfering chattermark trails (encircled with white).

SEM image of detrital quartz grain from beach sediment (Vår Haller, Sweden... Available to Purchase

Published: 01 February 2011
Figure 6 SEM image of detrital quartz grain from beach sediment (Vår Haller, Sweden, grain size = 520 μm). This quartz grain was also etched with dilute hydrofluoric acid (10%) for 25 minutes. It shows a high abundance of interfering chattermark trails (encircled with white).
Image
SEM image of detrital quartz grain from cave sediments (Bismarck cave in Franconia, Bavaria, Germany). The cave sediments are redeposited Cretaceous sands. The dimension of this detrital quartz grain is 155 μm x 100 μm. It shows a conchoidal broken surface with chattermark trails (encircled with white).

SEM image of detrital quartz grain from cave sediments (Bismarck cave in Fr... Available to Purchase

Published: 01 February 2011
Figure 1 SEM image of detrital quartz grain from cave sediments (Bismarck cave in Franconia, Bavaria, Germany). The cave sediments are redeposited Cretaceous sands. The dimension of this detrital quartz grain is 155 μm x 100 μm. It shows a conchoidal broken surface with chattermark trails
Image
Post-etching SEM image of a bead surface. Note the linear series of chattermark trails (one example is encircled with white) in addition to the scratches (same area as in Fig. 2). Some series are crossed by scratches as in Figure 2. The linear scratch is slightly wider compared to the unetched scratch in Figure 2. Alongside the scratch are some dust particles on top of the surface (surface is lit from the upper left).

Post-etching SEM image of a bead surface. Note the linear series of chatter... Available to Purchase

Published: 01 February 2011
Figure 3 Post-etching SEM image of a bead surface. Note the linear series of chattermark trails (one example is encircled with white) in addition to the scratches (same area as in Fig. 2 ). Some series are crossed by scratches as in Figure 2 . The linear scratch is slightly wider compared
Journal Article

Discussion Open Access

Published: 01 August 1993
Jour. Geol. Soc. India (1993) 42 (2): 199–202.
DOI: https://doi.org/10.17491/jgsi/1993/420209
... the nature of the accompanying textures, the circular pit in Plate 11-Figure 8 indicates a chemical origin. Deparr~nentof Earth Sciences Indian Insr iture of Technology .Powai, Bombay-400 076 RAVINDRANATA PRASAD Reference BULLP,. A., CULVERS., J. and GARDNBRR, . (L980) Chattermark trails...
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Journal Article

HERTZIAN FRACTURES IN THE SUB-DWYKA NOOITGEDACHT STRIATED PAVEMENT, AND IMPLICATIONS FOR THE FORMER THICKNESS OF KAROO STRATA NEAR KIMBERLEY, SOUTH AFRICA Available to Purchase

S. MASTER
Published: 01 December 2012
South African Journal of Geology (2012) 115 (4): 561–576.
DOI: https://doi.org/10.2113/gssajg.115.4.561
... and geochemical stratigraphy . Precambrian Research , 31 , 297 – 324 . Bull P.A. Culver S.J. Gardner R. , 1980 . Chattermark trails as paleoenvironmental indicators . Geology , 8 , 318 – 322 . Burshtein L.S. , 1968 . Determination of Poisson’s ratio of rocks by static...
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View PDF for article title, HERTZIAN FRACTURES IN THE SUB-DWYKA NOOITGEDACHT STRIATED PAVEMENT, AND IMPLICATIONS FOR THE FORMER THICKNESS OF KAROO STRATA NEAR KIMBERLEY, SOUTH AFRICA
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Journal Article

IMPRINTS IN SILICA GRAINS INDUCED DURING AN OPEN-CHANNEL FLOW EXPERIMENT: DETERMINATION OF MICROTEXTURAL SIGNATURES DURING AQUEOUS TRANSPORT Available to Purchase

PEDRO J.M. COSTA, YONG SUNG PARK, YOUNG DO KIM, MARIA QUINTELA, WILLIAM C. MAHANEY, FRANCISCO DOURADO, SUE DAWSON
Published: 01 July 2017
Journal of Sedimentary Research (2017) 87 (7): 677–687.
DOI: https://doi.org/10.2110/jsr.2017.39
... , p . 269 – 299 . Peterknecht, K.M., and Tietz, G.F., 2011 , Chattermark trails: surface features on detrital quartz grains indicative of a tropical climate : Journal of Sedimentary...
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View PDF for article title, IMPRINTS IN SILICA GRAINS INDUCED DURING AN OPEN-CHANNEL FLOW EXPERIMENT: DETERMINATION OF MICROTEXTURAL SIGNATURES DURING AQUEOUS TRANSPORT
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