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by M. Baba, J. Parnell, S. Bowden, J. Armstrong, M. Perez, and X. Wang

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Presentation on theme: "by M. Baba, J. Parnell, S. Bowden, J. Armstrong, M. Perez, and X. Wang"— Presentation transcript:

1 Emplacement of oil in the Devonian Weardale Granite of northern England
by M. Baba, J. Parnell, S. Bowden, J. Armstrong, M. Perez, and X. Wang Proceedings of the Yorkshire Geological Society Volume ():pygs February 22, 2019 © 2019 The Author(s). Published by The Geological Society of London for the Yorkshire Geological Society

2 Map of the Alston Block, northern Pennines, showing the limit of the buried Weardale Granite, the region of fluorite mineralization in the overlying limestone, and sample localities (after Bott & Masson Smith 1957). Map of the Alston Block, northern Pennines, showing the limit of the buried Weardale Granite, the region of fluorite mineralization in the overlying limestone, and sample localities (after Bott & Masson Smith 1957). M. Baba et al. Proceedings of the Yorkshire Geological Society 2018;pygs © 2019 The Author(s). Published by The Geological Society of London for the Yorkshire Geological Society

3 Segment of Rookhope Borehole core, depth 1647 feet (502 m), consisting of Weardale Granite cut by bitumen-bearing quartz vein (dark) mineralized by pyrite. Segment of Rookhope Borehole core, depth 1647 feet (502 m), consisting of Weardale Granite cut by bitumen-bearing quartz vein (dark) mineralized by pyrite. The quartz-bitumen vein is cut by a thin fluorite-bearing vein. M. Baba et al. Proceedings of the Yorkshire Geological Society 2018;pygs © 2019 The Author(s). Published by The Geological Society of London for the Yorkshire Geological Society

4 Thin section photomicrograph of bitumen (black) interstitial to quartz in the Weardale Granite, depth 1686 feet (514 m) in the Rookhope Borehole. Thin section photomicrograph of bitumen (black) interstitial to quartz in the Weardale Granite, depth 1686 feet (514 m) in the Rookhope Borehole. M. Baba et al. Proceedings of the Yorkshire Geological Society 2018;pygs © 2019 The Author(s). Published by The Geological Society of London for the Yorkshire Geological Society

5 Mass fragmentograms for m/z 85 for bitumen samples from the Weardale Granite (Rookhope Borehole) and Carboniferous limestone (Moot Law). Mass fragmentograms for m/z 85 for bitumen samples from the Weardale Granite (Rookhope Borehole) and Carboniferous limestone (Moot Law). M. Baba et al. Proceedings of the Yorkshire Geological Society 2018;pygs © 2019 The Author(s). Published by The Geological Society of London for the Yorkshire Geological Society

6 Mass fragmentograms for m/z 217 for bitumen samples from the Weardale Granite (Rookhope Borehole) and Carboniferous limestone (Moot Law). Mass fragmentograms for m/z 217 for bitumen samples from the Weardale Granite (Rookhope Borehole) and Carboniferous limestone (Moot Law). M. Baba et al. Proceedings of the Yorkshire Geological Society 2018;pygs © 2019 The Author(s). Published by The Geological Society of London for the Yorkshire Geological Society

7 Composition of C27, C28 and C29 steranes (αββ S + R) in samples from the Weardale Granite, from Moot Law, and from shale at the surface at Rookhope. Composition of C27, C28 and C29 steranes (αββ S + R) in samples from the Weardale Granite, from Moot Law, and from shale at the surface at Rookhope. Data determined from m/z 218 chromatograms. Compositions cluster between C27 and C29 predominance. M. Baba et al. Proceedings of the Yorkshire Geological Society 2018;pygs © 2019 The Author(s). Published by The Geological Society of London for the Yorkshire Geological Society

8 Cross-plot of homogenization temperature (Th) against final ice melting temperature (Tm) for granite-hosted phases and fluorite in limestone. Cross-plot of homogenization temperature (Th) against final ice melting temperature (Tm) for granite-hosted phases and fluorite in limestone. M. Baba et al. Proceedings of the Yorkshire Geological Society 2018;pygs © 2019 The Author(s). Published by The Geological Society of London for the Yorkshire Geological Society

9 LA-ICP-MS element maps for a pyrite crystal in a bitumen-bearing quartz vein (Fig. 2) in the Weardale Granite. LA-ICP-MS element maps for a pyrite crystal in a bitumen-bearing quartz vein (Fig. 2) in the Weardale Granite. Note pyrite is enriched in trace elements including Au, Ag, Se and Te. M. Baba et al. Proceedings of the Yorkshire Geological Society 2018;pygs © 2019 The Author(s). Published by The Geological Society of London for the Yorkshire Geological Society

10 Cross-plot of Au and Se in pyrite from the Weardale Granite in the Rookhope Borehole and from mining waste from Allenheads, measured from LA-ICP-MS. Cross-plot of Au and Se in pyrite from the Weardale Granite in the Rookhope Borehole and from mining waste from Allenheads, measured from LA-ICP-MS. Pyrite from the Weardale Granite consistently shows higher Au and Se contents. M. Baba et al. Proceedings of the Yorkshire Geological Society 2018;pygs © 2019 The Author(s). Published by The Geological Society of London for the Yorkshire Geological Society


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