Publications
Found 486 results
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Minimal geological methane emissions during the Younger Dryas–Preboreal abrupt warming event. Nature. 548:443–446.
. 2017. Minimal geological methane emissions during the Younger Dryas–Preboreal abrupt warming event. Nature. 548:443–446.
. 2017. Minimal geological methane emissions during the Younger Dryas–Preboreal abrupt warming event. Nature. 548:443–446.
. 2017. Minimal geological methane emissions during the Younger Dryas–Preboreal abrupt warming event. Nature. 548:443–446.
. 2017. Minimal geological methane emissions during the Younger Dryas–Preboreal abrupt warming event. Nature. 548:443–446.
. 2017. Modelling firn thickness evolution during the last deglaciation: constraints on sensitivity to temperature and impurities. Climate of the Past. 13:833–833.
. 2017. Modelling firn thickness evolution during the last deglaciation: constraints on sensitivity to temperature and impurities. Climate of the Past. 13:833–833.
. 2017. Molybdenum (Mo) stable isotopic variations as indicators of Mo attenuation in mine waste-rock drainage. Applied Geochemistry. In Press
. 2017. Molybdenum (Mo) stable isotopic variations as indicators of Mo attenuation in mine waste-rock drainage. Applied Geochemistry. 87:71–83.
. 2017. Quantifying the volcanic emissions which triggered Oceanic Anoxic Event 1a and their effect on ocean acidification. Sedimentology. 64:204-214.
. 2017. The recent warming trend in North Greenland. Geophysical Research Letters. 44:6235–6243.
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Constraining the transport time of lithogenic sediments to the Okinawa Trough (East China Sea). Chemical Geology. 445:199-207.
. 2016. Constraining the transport time of lithogenic sediments to the Okinawa Trough (East China Sea). Chemical ….
. 2016. . 2016. How warm was Greenland during the last interglacial period? Climate of the Past. 12:1933–1948.
. 2016. How warm was Greenland during the last interglacial period? Climate of the Past. 12:1933–1948.
. 2016. Hydrothermal alteration revealed by apatite luminescence and chemistry: a potential indicator mineral for exploring covered porphyry copper deposits. Economic Geology. 111:1397–1410.
. 2016. Hydrothermal alteration revealed by apatite luminescence and chemistry: a potential indicator mineral for exploring covered porphyry copper deposits. Economic Geology. 111:1397–1410.
. 2016. Hydrothermal alteration revealed by apatite luminescence and chemistry: a potential indicator mineral for exploring covered porphyry copper deposits. Economic Geology. 111:1397–1410.
. 2016. . 2016. . 2016.