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iron-stained

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Journal Article
Published: 10 February 2010
Geological Magazine (2010) 147 (5): 728–736.
...BRENT WILSON Abstract Eleven samples of seafloor sediment were taken from water depths of 78–90 m within the Savonette Field, off SE Trinidad, western Atlantic Ocean. This surface sediment is relict, having been deposited during an early Holocene transgression. The samples yielded much iron-stained...
Journal Article
Published: 01 November 1975
Clays and Clay Minerals (1975) 23 (5): 355–360.
Journal Article
Published: 09 April 2014
Geological Magazine (2015) 152 (1): 1–11.
... Chalk Formation are sites of localized syndepositional iron staining. These nodules are not stromatolitic or microbial and are not evidence for deposition in shallow-water or intertidal settings. † Author for correspondence: [email protected] 15 08 2013 12 02 2014 Copyright ©...
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First thumbnail for: Microbial crust with Frutexites (?) and <span clas...
Second thumbnail for: Microbial crust with Frutexites (?) and <span clas...
Third thumbnail for: Microbial crust with Frutexites (?) and <span clas...
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Light-orange, iron-stained Gossan Peak within light-coloured, quartz–mica schist of Healy schist, which weathers buff to tan, viewed looking northeast from location 05ADb37 (No. 5 in Fig. 2). Photograph by C.R. Bacon, US Geological Survey.
Published: 19 December 2023
Fig. 5. Light-orange, iron-stained Gossan Peak within light-coloured, quartz–mica schist of Healy schist, which weathers buff to tan, viewed looking northeast from location 05ADb37 (No. 5 in Fig. 2 ). Photograph by C.R. Bacon, US Geological Survey.
Image
Core fragmentation through moderately to heavily orange, iron-stained and partly filled multiple vertical open fractures (CIRIA grade C) in the Seaford Chalk Formation. (b) is a close-up of (a) and (d) is a close-up of (c).
Published: 22 July 2021
Fig. 3. Core fragmentation through moderately to heavily orange, iron-stained and partly filled multiple vertical open fractures (CIRIA grade C) in the Seaford Chalk Formation. ( b ) is a close-up of ( a ) and ( d ) is a close-up of ( c ).
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(a) Brown iron stained aggregate in (10% silicate solution) silica gel (exp. 1). (b) Red impurity in agate. (Online version in colour.)
Published: 01 January 2018
Fig. 9 (a) Brown iron stained aggregate in (10% silicate solution) silica gel (exp. 1). (b) Red impurity in agate. (Online version in colour.)
Image
A View across Pebble West zone looking east. Iron-stained rubble crop in foreground with naturally acidic ponds behind. Shaded hill in center distance is till ridge overlying the Pebble East zone. B. Looking northwest across glacial features over the deeply concealed Pebble East zone. Slope of lateral moraine in foreground. Ponds in (B) have circumneutral pH. Photos by R.G. Eppinger.
Published: 01 May 2013
Fig. 2 A View across Pebble West zone looking east. Iron-stained rubble crop in foreground with naturally acidic ponds behind. Shaded hill in center distance is till ridge overlying the Pebble East zone. B. Looking northwest across glacial features over the deeply concealed Pebble East zone
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A View across Pebble West zone looking east. Iron-stained rubble crop in foreground with naturally acidic ponds behind. Shaded hill in center distance is till ridge overlying the Pebble East zone. B. Looking northwest across glacial features over the deeply concealed Pebble East zone. Slope of lateral moraine in foreground. Ponds in (B) have circumneutral pH. Photos by R.G. Eppinger.
Published: 01 May 2013
Fig. 2 A View across Pebble West zone looking east. Iron-stained rubble crop in foreground with naturally acidic ponds behind. Shaded hill in center distance is till ridge overlying the Pebble East zone. B. Looking northwest across glacial features over the deeply concealed Pebble East zone
Image
Distribution of iron-stained features in the Chalk based on re-logging chalk cores (Harris, 1998) compared with the stratigraphic ground model (Mortimore 1993b, 1994). This illustrates the concentration of such features associated with slickensided fractures in the Newhaven Chalk Formation and the fault zones, and the concentration of stained subhorizontal features in the Seaford Chalk formation that had been suggested by Mortimore (1993b).
Published: 01 August 2012
Fig. 112. Distribution of iron-stained features in the Chalk based on re-logging chalk cores ( Harris, 1998 ) compared with the stratigraphic ground model ( Mortimore 1993 b , 1994 ). This illustrates the concentration of such features associated with slickensided fractures in the Newhaven
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Iron-stained, cross-bedded sandstones of the Adaffa Formation (Suqah Group); Midyan Basin (28°05′48.5″N, 35°16′02.6″E). These sediments contain petrified wood, phosphatic nodules and fossilized dinosaur bones.
Published: 01 July 2005
Figure 8: Iron-stained, cross-bedded sandstones of the Adaffa Formation (Suqah Group); Midyan Basin (28°05′48.5″N, 35°16′02.6″E). These sediments contain petrified wood, phosphatic nodules and fossilized dinosaur bones.
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Lateral distribution of: A, iron-stained quartz; B, shell fragments (in 1-2 mm fraction); and C, fauna on Sable Island Bank. Contours in fathoms.
Published: 01 November 1968
Fig. 6 Lateral distribution of: A, iron-stained quartz; B, shell fragments (in 1-2 mm fraction); and C, fauna on Sable Island Bank. Contours in fathoms.
Image
—Numerous angular quartz grains in iron-stained carbonate matrix, diameter 1.8 mm., upper unit, Sloss and Laird’s beds of undetermined age, Logan section B.
Published: 01 November 1950
FIG. 4. —Numerous angular quartz grains in iron-stained carbonate matrix, diameter 1.8 mm., upper unit, Sloss and Laird’s beds of undetermined age, Logan section B.
Journal Article
Journal: GSA Bulletin
Published: 01 March 1972
GSA Bulletin (1972) 83 (3): 877–884.
...DONALD J. P SWIFT; W. RICHARD BOEHMER Abstract Brown iron-staining on coarse shelf sands has been taken as evidence of subaerial weathering, either in the source area or at the depositional site. However, we note that iron-staining can occur subaqueously, as well. We have found a close correlation...
Journal Article
Published: 01 June 1970
American Mineralogist (1970) 55 (5-6): 1048–1051.
...Marco T. Einaudi Abstract An ammonium dichromate-hydrochloric acid solution serves as an iron-sensitive stain on polished surfaces of iron-rich sphalerite. Copyright © 1970 by the Mineralogical Society of America 1970 Mineralogical Society of America ...
Image
Conglomerates and sandstones of the Adaffa Formation note iron staining (arrow). Located at 28°05′48.5″N, 35°16′02.6″E; view looking north. Width of photo about 12 m.
Published: 01 July 2005
Figure 7: Conglomerates and sandstones of the Adaffa Formation note iron staining (arrow). Located at 28°05′48.5″N, 35°16′02.6″E; view looking north. Width of photo about 12 m.
Journal Article
Published: 01 November 1988
Quarterly Journal of Engineering Geology and Hydrogeology (1988) 21 (4): 361–369.
...G. Davies; R. E. Oberholster Abstract Problems of pop-outs and associated iron staining on unplastered clinker ash/cement brick walls in Windhoek after a particularly wet rainy season were investigated. The problems were found to be due to sulphurous nodules present in the bricks. The nodules were...
Journal Article
Published: 01 September 2017
Journal of Sedimentary Research (2017) 87 (9): 951–966.
... deposits comprise iron-stained and chloritic siltstones that contain iron-stained and phosphatic ooids, phosphatic pebbles, and fragmented and abraded body fossils (facies association D); these deposits record prolonged physical reworking, winnowing, and sediment bypass. The long-term progradation rate...
FIGURES
First thumbnail for: Sedimentologic Character of Ancient Muddy Subaqueo...
Second thumbnail for: Sedimentologic Character of Ancient Muddy Subaqueo...
Third thumbnail for: Sedimentologic Character of Ancient Muddy Subaqueo...
Journal Article
Published: 01 December 1970
American Mineralogist (1970) 55 (11-12): 2134.
Journal Article
Published: 01 June 1975
Journal of Sedimentary Research (1975) 45 (2): 541–542.
...Sheldon Sommer Abstract Microprobe determination of carbonates stained with reagents utilized in the determination of iron show marked depletion in iron content as compared to unstained areas. Removal of iron to the solution by potassium ferricynide in an acid medium must be taken...
Journal Article
Published: 01 March 1972
Journal of Sedimentary Research (1972) 42 (1): 239–242.
...R. C. Lindholm; R. B. Finkelman Abstract Calcite phases with different amounts of ferrous iron (determined by microprobe analysis) are distinguishable by study of stained thin sections and stained acetate peels. We have defined four such phases, they are (a) non-ferroan calcite (0.0% FeO; red stain...