Quartz cementation history of sandstones revealed by high resolution SIMS oxygen isotope analysis
(2013)
Journal Article
Harwood, J., Aplin, A., Fialips, C., Iliffe, J., Kozdon, R., Ushikubo, T., & Valley, J. (2013). Quartz cementation history of sandstones revealed by high resolution SIMS oxygen isotope analysis. Journal of Sedimentary Research, 83(7), 522-530. https://doi.org/10.2110/jsr.2013.29
Andrew Aplin's Outputs (4)
Mercia Mudstone Formation caprock to carbon capture and storage sites: petrology and petrophysical characteristics (2013)
Journal Article
Armitage, P., Worden, R., Faulkner, D., Aplin, A., Butcher, A., & Espie, A. (2013). Mercia Mudstone Formation caprock to carbon capture and storage sites: petrology and petrophysical characteristics. Journal of the Geological Society, 170(1), 119-132. https://doi.org/10.1144/jgs2012-049
FIB-SEM and TEM investigations of an organic-rich shale maturation series (Lower Toarcian Posidonia Shale): Nanoscale pore system and fluid-rock interactions (2013)
Book Chapter
Bernard, S., Wirth, R., Schreiber, A., Bowen, L., Aplin, A., Mathia, E., …Horsfield, B. (2013). FIB-SEM and TEM investigations of an organic-rich shale maturation series (Lower Toarcian Posidonia Shale): Nanoscale pore system and fluid-rock interactions. In W. Camp, E. Diaz, & B. Wawak (Eds.), Electron microscopy of shale hydrocarbon reservoirs (53-66). AAPG
Methane adsorption on shale under simulated geological temperature and pressure conditions (2013)
Journal Article
Rexer, T., Benham, M., Aplin, A., & Thomas, K. (2013). Methane adsorption on shale under simulated geological temperature and pressure conditions. Energy and Fuels, 27(6), 3099-3109. https://doi.org/10.1021/ef400381vShale gas is becoming an increasingly important energy resource. In this study, the adsorption of methane on a dry, organic-rich Alum shale sample was studied at pressures up to 14 MPa and temperatures in the range 300–473 K, which are relevant to ga... Read More about Methane adsorption on shale under simulated geological temperature and pressure conditions.