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Unique Identification: Dolomite
Site name: not specified
Light type: Plane-Polarized Light
Magnification: not specified
Submitted by: Guy Rothwell
Notes: Euhedral dolomite rhomb, rhombic
Image Tags: none
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Unique Identification: Dolomite
Site name: Pyramid
Light type: Plane-Polarized Light
Magnification: 400X
Submitted by: Joe Smoot
Notes: high relief, rhombic
Image Tags: none
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Unique Identification: Dolomite
Site name: Pyramid
Light type: Cross-Polarized Light
Magnification: 400X
Submitted by: Joe Smoot
Notes: high birefringence, rhombic
Image Tags: none
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Unique Identification: Dolomite
Site name: Lake Bosumtwi
Light type: Plane-Polarized Light
Magnification: not specified
Submitted by: not specified
Notes: none
Image Tags: none
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Unique Identification: Dolomite
Site name: Lake Bosumtwi
Light type: Cross-Polarized Light
Magnification: not specified
Submitted by: not specified
Notes: none
Image Tags: none
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Unique Identification: Dolomite
Site name: Bosumtwi
Light type: Plane-Polarized Light
Magnification: 630X
Submitted by: Michael Rosen Blas Valero
Notes: corroded rhombic transparent high-birefringent
Image Tags: none
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Unique Identification: Dolomite
Site name: Bosumtwi
Light type: Cross-Polarized Light
Magnification: 630X
Submitted by: Michael Rosen Blas Valero
Notes: corroded rhombic transparent high-birefringent
Image Tags: none
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Unique Identification: Dolomite
Site name: Bosumtwi
Light type: Plane-Polarized Light
Magnification: 630X
Submitted by: Michael Rosen Blas Valero
Notes: rhombic transparent high-birefringent
Image Tags: none
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Unique Identification: Dolomite
Site name: Bosumtwi
Light type: Cross-Polarized Light
Magnification: 630X
Submitted by: Michael Rosen Blas Valero
Notes: euhedral, rhombic transparent high-birefringent
Image Tags: none
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Unique Identification: Dolomite
Site name: Red Lake Peatland
Light type: Scanning Electron Micrograph
Magnification: 1200.0
Submitted by: Mark Shapley
Notes: Detrital dolomite (composition confirmed by EDX) from beneath a peatland. The denticulate texture is interpreted as the result of partial dissolution in a low-pH depositional environment. Through the petrographic microscope, partially dissolved carbonate mineral grains may exhibit prominent 'zig-zag' patterning to birefringence, due to etching along cleavage planes and grain boundaries.
Image Tags: detrital toothed dissolution etched ragged reaction-texture SEM resorbed
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Unique Identification: Dolomite
Site name: Red Lake Peatland
Light type: Scanning Electron Micrograph
Magnification: 1500.0
Submitted by: Mark Shapley
Notes: Detrital dolomite (composition confirmed by EDX) from beneath a peatland. The denticulate texture is interpreted as the result of partial dissolution in a low-pH depositional environment. Through the petrographic microscope, partially dissolved carbonate mineral grains may exhibit prominent 'zig-zag' patterning to birefringence, due to etching along cleavage planes and grain boundaries.
Image Tags: detrital toothed dissolution etched ragged reaction-texture SEM resorbed
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Unique Identification: Dolomite
Site name: Red Lake Peatland
Light type: Scanning Electron Micrograph
Magnification: 1200.0
Submitted by: Mark Shapley
Notes: Detrital dolomite (composition confirmed by EDX) from beneath a peatland. The denticulate texture is interpreted as the result of partial dissolution in a low-pH depositional environment. Through the petrographic microscope, partially dissolved carbonate mineral grains may exhibit prominent 'zig-zag' patterning to birefringence, due to etching along cleavage planes and grain boundaries.
Image Tags: detrital toothed dissolution etched ragged reaction-texture SEM resorbed
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Unique Identification: Dolomite
Site name: Red Lake Peatland
Light type: Scanning Electron Micrograph
Magnification: 5000.0
Submitted by: Mark Shapley
Notes: Detrital dolomite (composition confirmed by EDX) from beneath a peatland. The denticulate texture is interpreted as the result of partial dissolution in a low-pH depositional environment. Through the petrographic microscope, partially dissolved carbonate mineral grains may exhibit prominent 'zig-zag' patterning to birefringence, due to etching along cleavage planes and grain boundaries.
Image Tags: detrital toothed dissolution etched ragged reaction-texture SEM resorbed
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Unique Identification: Dolomite
Site name: Red Lake Peatland
Light type: Scanning Electron Micrograph
Magnification: 1800.0
Submitted by: Mark Shapley
Notes: Detrital dolomite (composition confirmed by EDX) from beneath a peatland. The denticulate texture is interpreted as the result of partial dissolution in a low-pH depositional environment. Through the petrographic microscope, partially dissolved carbonate mineral grains may exhibit prominent 'zig-zag' patterning to birefringence, due to etching along cleavage planes and grain boundaries.
Image Tags: detrital toothed dissolution etched ragged reaction-texture SEM resorbed
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