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Geology & Geophysics Guide to Borehole Core in the Karoo Basin ...

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<strong>Geology</strong> & <strong>Geophysics</strong><br />

<strong>Guide</strong> <strong>to</strong> <strong>Borehole</strong> <strong>Core</strong><br />

<strong>in</strong> <strong>the</strong> <strong>Karoo</strong> Bas<strong>in</strong> Coalfields<br />

South Africa<br />

(<strong>in</strong>terim report)<br />

Bruce Cairncross (PhD)<br />

Head: Department of <strong>Geology</strong><br />

University of Johannesburg


Wh Why? ?<br />

Provide a colour pho<strong>to</strong>graphic guide of typical<br />

borehole core samples from <strong>the</strong> <strong>Karoo</strong> Bas<strong>in</strong><br />

coalfields <strong>to</strong>:<br />

:<br />

- Standardize descriptions when logg<strong>in</strong>g core<br />

- Assist geologists, geotechnicians, drillers,<br />

samplers samplers, etc <strong>in</strong> recognis<strong>in</strong>g common features<br />

such as rock type and sedimentary structures<br />

<strong>in</strong> borehole core.


Cross-bedded sands<strong>to</strong>ne<br />

Matrix-supported conglomerate


Bioturbated silts<strong>to</strong>ne/sands<strong>to</strong>ne<br />

(50 core samples pho<strong>to</strong>graphed <strong>to</strong>-date) <strong>to</strong> date)


Eng<strong>in</strong>eer<strong>in</strong>g <strong>Geology</strong> 64 (2002) 19–39<br />

“A geomechanical survey of some different facies <strong>in</strong> relation <strong>to</strong><br />

stability at a m<strong>in</strong>e <strong>in</strong> <strong>the</strong> Eastern Transvaal Coalfield, South Africa”<br />

F.G. Bell*, C.A. Jermy<br />

DDepartment t t of f <strong>Geology</strong> G l and dA Applied li d G<strong>Geology</strong>, l<br />

University of Natal, Durban, 4041, South Africa<br />

“In particular, poor roof and floor conditions were found <strong>to</strong> be<br />

associated with rocks of <strong>the</strong> argillaceous facies. The most<br />

stable t bl strata t t were <strong>the</strong> th f<strong>in</strong>e-gra<strong>in</strong>ed fi i d arenaceous facies f i whilst hil t<br />

those of <strong>the</strong> coarse-gra<strong>in</strong>ed facies were somewhat less<br />

stable”.


Poor roof / floor<br />

conditions<br />

di i


Stable roof / floor conditions


Interstate highway road-cut,<br />

KKentucky, t k USA USA(A (Appalachian l hi coalfields) lfi ld )<br />

Flat bedded sands<strong>to</strong>ne with <strong>in</strong>terlayered silts<strong>to</strong>ne


Carboniferous coalfields, Alabama, USA


Record<strong>in</strong>g Gra<strong>in</strong> size <strong>in</strong> Sedimentary Rocks<br />

Üdden‐Wentworth Clastic Sediment Gra<strong>in</strong>‐size Chart<br />

mm diameter Name<br />

(above 256) Boulders<br />

256<br />

128<br />

Cobbles<br />

64<br />

Gravel<br />

32<br />

16<br />

(rock equivalent = conglomerate)<br />

8<br />

4<br />

Pebbles<br />

2 Granules Granules<strong>to</strong>ne (“grits<strong>to</strong>ne”)<br />

1 Very coarse sand<br />

0.5 Coarse sand<br />

0.25 Medium sand<br />

0.125 F<strong>in</strong>e sand<br />

0.063 Very f<strong>in</strong>e sand<br />

00.031 031 Coarse silt<br />

0.0156 Medium silt<br />

0.0078 F<strong>in</strong>e silt<br />

00.0039 0039 Very f<strong>in</strong>e silt<br />

(less than 0.0039) Clay<br />

Sand<br />

(rock equivalent = sands<strong>to</strong>ne)<br />

Mud<br />

(rock equivalent = muds<strong>to</strong>ne;<br />

<strong>in</strong>cludes silts<strong>to</strong>ne and shale)


The borehole core samples illustrated here are<br />

colour coded for easy reference:<br />

GREY = Muds<strong>to</strong>ne (<strong>in</strong>clud<strong>in</strong>g shale and<br />

silts<strong>to</strong>ne)<br />

RED = <strong>in</strong>terlayered muds<strong>to</strong>ne<br />

and sands<strong>to</strong>ne<br />

YELLOW = Sands<strong>to</strong>ne<br />

BLUE = conglomerate<br />

GREEN = deformed strata<br />

PURPLE PURP = igneous rocks (dolerite)


Academic / Scientific Reasons for a standardized core log book<br />

Interpret<strong>in</strong>g <strong>the</strong> environments of formation of <strong>the</strong> rocks conta<strong>in</strong><strong>in</strong>g <strong>the</strong><br />

p g g<br />

coal (different coal types and coal distributionsassociated with different<br />

depositional environments)


Mississippi Delta (River (River-dom<strong>in</strong>ated dom<strong>in</strong>ated delta)


Bedload Fluvial<br />

Facies Assemblage g


<strong>Borehole</strong> <strong>Core</strong> Supplied by<br />

Project Sponsored by

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