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Some pits are fresh, exposed by recent removal of the sedimentary coating and fossilised bone surface.
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Open image in new window Fig. 3 Comparison of grain-coating chlorite content in different sedimentary microfacies, including: underwater distributary channels, distributary channels, mouth bars, and shallow lake sandstone dams.
Grain-coating chlorite formation was thought to be mainly controlled by sedimentary facies and formed in high hydrodynamic conditions and weak alkaline environments with abundant Fe and Al sources (Huang et al. 2004).
Authigenic grain-coating chlorite is widely distributed in the clastic rocks of many sedimentary basins around the world.
Grain-coating chlorite, also known as pore-lining chlorite, is widely distributed in many sedimentary basins around the world.
Sand bodies with authigenic grain-coating chlorite in the study area may be divided into four types of sedimentary microfacies: underwater distributary channels, distributary channel, shallow lake sandstone dams, and mouth bars.
Sedimentary rock interacts with rainwater.
Prologue, Scene 6 is Introducing Sedimentary Rocks.
"Sedimentary layers are what people understand".
Not all sedimentary deposits are stratified.
For full treatment, see sedimentary rock: Evaporites.
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