"A transparent, multi-proxy desk screen—barium–rubidium
stream-sediment geochemistry (a proxy for the Altar Stone’s diagnostic baryte
cement and K-feldspar deficit), thermal-maturity mapping, clay mineralogy,
sedimentary facies, and detrital-zircon provenance—has been applied iteratively
across the UK Old Red Sandstone (ORS). It has narrowed a national-scale
problem, step by step and at the appropriate level of evidence, to a single
field-accessible target. The screen and Clarke et al.’s (2024, 2026) detrital-zircon
data agree that the source lies on the East Caithness coast; but the prime
barium cluster (Sarclet–Lybster–Clyth) sits in the high-maturity zone mapped by
Hillier & Marshall (1992), where vitrinite reflectance of 3–6% R₀
has driven the delicate expandable and aluminous clays of the Altar Stone past
preservation.
Two
independent lines then refine, rather than defeat, the result. The clay
evidence (Hillier & Clayton 1989; Hillier et al. 2006) shows the Altar
Stone’s tosudite–kaolinite–dioctahedral-chlorite assemblage to be an aluminous
sandstone diagenetic pathway. While classically expressed in the UK Lower ORS,
work on offshore Middle Devonian blocks (e.g., the Clair Group) demonstrates
that this signature is strictly facies- and fluid-controlled rather than
stratigraphically restricted, meaning it can be seamlessly accommodated within
porous sandstone bodies encased in lower-maturity segments of the Caithness
Flagstone Group.
One place is identified where such a rock could occur:"
I've included a photo of a megalithic monument that is there, but I need to just check it again before revealing the site.
The main problem is that the lack of data means that unsampled gaps in the record don't get filtered out, and that small areas are filtered out by being smeared in with the surrounding geology. Other data may highlight such areas, and suggest better screening. So such a desktop screening exercise can only suggest places worth further investigation, with a rock hammer.
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