Sedimentology of mud - Canadian Society of Petroleum Geologists

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Greenhorn Formation, Cenomanian - Turonian (Kansas) Silt-bearing clay-rich calcareous mudstones. Foraminifer, pellets and aggregate grains form the silt-sized fraction RKB#1 1006.7 RKB#1 1006.7
Looking in the dark: key observations a) All these mudstone units (classic source rock intervals) are very heterogeneous at scales ranging from 10 -2 m to 10 -5 m. b) They are organized into stacked succession of very thin beds (typically each
Page 1 and 2: Are shales really that dull? Shinin
Page 3 and 4: Before I start I would like to than
Page 5 and 6: Real World Observations: sub-log sc
Page 7 and 8: Real World Observations: sub-log sc
Page 9 and 10: Current paradigm for sediment trans
Page 11 and 12: Kimmeridge Clay Formation All KCF s
Page 13 and 14: Kimmeridge Clay Formation >TOC in i
Page 15 and 16: Kimmeridge Clay Formation Normally
Page 17 and 18: Kimmeridge Clay Formation Stacked s
Page 19 and 20: Kimmeridge Clay Formation Horizonta
Page 21 and 22: Shining more light into dark places
Page 23 and 24: Mulgrave Shale Member Sharp based,
Page 25 and 26: Mulgrave Shale Member Normally grad
Page 27 and 28: Mulgrave Shale Member BSEI image, d
Page 29 and 30: Mulgrave Shale Member Sub-horizonta
Page 31 and 32: Grey Shale Member Normally graded b
Page 33 and 34: Mulgrave Shale Member Normally grad
Page 35 and 36: Second White Speckled Shale Member,
Page 37 and 38: Second White Speckled Shale Member,
Page 39: Greenhorn Formation, Cenomanian - T
Page 43 and 44: Wave enhanced gravity flows of flui
Page 45 and 46: These fabrics are commonly encounte
Page 47 and 48: Ripple laminae composed of intercal
Page 49 and 50: Micro-textures in the Jet Rock MCO2
Page 51 and 52: Suspension settling processes. •
Page 53 and 54: Microfabric data and the effects of
Page 55 and 56: Where do we go now, now that Pandor
Page 57: References - to current research Al

Sedimentology of mud - Canadian Society of Petroleum Geologists

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