REINTERPRETATION OF MT NEBO POINTE SAND INJECTITE COMPLEX, PITTSBURGH, PA
Petrographic analysis of oriented samples showed the inter-crack sandstone and the host rock exhibit the same mineralogy, subhorizontal grain trends and grain packing. Close examination of the highwall revealed that some cracks contain horizontal muscovite-rich weathering planes concordant with bounding surfaces. Conversely, a sand injectite hypothesis would predict the material to be of different composition with clear dike-parallel grain trends, tight packing and truncation of host sedimentary structures. Only one sample showed any vertical trends, appearing to grade laterally from coarse to fine sand.
However, the mineralogy does suggest pervasive oxidative diagenesis related to fluid flow. Chlorite grains and iron oxide cement account for 15% and 3% of the host rock respectively, while the inter-crack sandstone contains up to 25% chlorite, ubiquitous iron oxide cement and increased secondary porosity. Muscovite and biotite are important accessories in all samples, and kaolinite is a minor accessory. Throughout the highwall, zones within and immediate to fractures are dominated by iron-oxide cement and Liesegang bands. A sharp “bathtub ring,” seen approximately six meters from the base, may indicate the maximum saturation level.
The distribution of crack morphologies does not appear to be associated with the highwall’s excavation. Cracks in the flanks tend to fan upwards while those nearer the center are linear and subvertical, even where overburden is minimal. It seems more likely this is linked to the joints’ proximity to the surface during either their formation or oxidation.
In light of these results, the term “dike” previously and tentatively used to describe these features is now considered an inaccurate genetic description.