https://ogma.newcastle.edu.au/vital/access/ /manager/Index en-au 5 https://ogma.newcastle.edu.au/vital/access/ /manager/Repository/uon:1937 Wed 24 Jul 2013 22:53:35 AEST ]]> https://ogma.newcastle.edu.au/vital/access/ /manager/Repository/uon:3222 Wed 24 Jul 2013 22:20:07 AEST ]]> https://ogma.newcastle.edu.au/vital/access/ /manager/Repository/uon:3212 Wed 11 Apr 2018 16:49:24 AEST ]]> https://ogma.newcastle.edu.au/vital/access/ /manager/Repository/uon:2989 Wed 11 Apr 2018 16:15:18 AEST ]]> https://ogma.newcastle.edu.au/vital/access/ /manager/Repository/uon:2988 Sat 24 Mar 2018 10:42:11 AEDT ]]> https://ogma.newcastle.edu.au/vital/access/ /manager/Repository/uon:1930 Sat 24 Mar 2018 08:33:20 AEDT ]]> https://ogma.newcastle.edu.au/vital/access/ /manager/Repository/uon:1961 Sat 24 Mar 2018 08:33:13 AEDT ]]> https://ogma.newcastle.edu.au/vital/access/ /manager/Repository/uon:1884 Sat 24 Mar 2018 08:31:18 AEDT ]]> https://ogma.newcastle.edu.au/vital/access/ /manager/Repository/uon:1538 Sat 24 Mar 2018 08:30:48 AEDT ]]> https://ogma.newcastle.edu.au/vital/access/ /manager/Repository/uon:1577 Sat 24 Mar 2018 08:30:29 AEDT ]]> https://ogma.newcastle.edu.au/vital/access/ /manager/Repository/uon:2817 Sat 24 Mar 2018 08:30:17 AEDT ]]> https://ogma.newcastle.edu.au/vital/access/ /manager/Repository/uon:1481 1 kg lost) or weight stable (≤1 kg lost) after an 8 week nutrition intervention period. Group survival duration (Kaplan Meier) and QoL (EORTC QLQ-C30) were compared. Predictors of weight stability were determined using logistic regression analysis. Results: Patients with weight stabilisation survived longer from baseline (log rank test 5.53, P=0.019). They also reported higher QoL scores (P=0.037) and a greater mean energy intake (P<0.001) at Week 8 than those who continued to lose weight. The absence of nausea and vomiting (OR 6.5, P=0.010) and female gender (OR 5.2, P=0.020) were independent determinants of weight stabilisation. Conclusions: Weight stabilisation over an 8 week period in weight-losing patients with unresectable pancreatic cancer was associated with improved survival duration and QoL.]]> Sat 24 Mar 2018 08:28:12 AEDT ]]> https://ogma.newcastle.edu.au/vital/access/ /manager/Repository/uon:1807 Sat 24 Mar 2018 08:27:34 AEDT ]]> https://ogma.newcastle.edu.au/vital/access/ /manager/Repository/uon:1739 Sat 24 Mar 2018 08:27:29 AEDT ]]> https://ogma.newcastle.edu.au/vital/access/ /manager/Repository/uon:1752 Sat 24 Mar 2018 08:27:25 AEDT ]]> https://ogma.newcastle.edu.au/vital/access/ /manager/Repository/uon:1987 Sat 24 Mar 2018 08:27:09 AEDT ]]> https://ogma.newcastle.edu.au/vital/access/ /manager/Repository/uon:3327 Sat 24 Mar 2018 07:23:19 AEDT ]]> https://ogma.newcastle.edu.au/vital/access/ /manager/Repository/uon:3681 Sat 24 Mar 2018 07:23:03 AEDT ]]> https://ogma.newcastle.edu.au/vital/access/ /manager/Repository/uon:3424 Sat 24 Mar 2018 07:21:37 AEDT ]]> https://ogma.newcastle.edu.au/vital/access/ /manager/Repository/uon:3266 Sat 24 Mar 2018 07:21:22 AEDT ]]> https://ogma.newcastle.edu.au/vital/access/ /manager/Repository/uon:3428 Sat 24 Mar 2018 07:20:26 AEDT ]]> https://ogma.newcastle.edu.au/vital/access/ /manager/Repository/uon:3434 100 K/s. Despite the existence of four other titanium silicides (TiSi₂, TiSi, Ti₅Si₄, Ti₃Si) evidence of these or other intermediate phases was not found in either the pre-heating or reaction stages of the process. The reaction is, however, narrowly preceded by the α→β transformation in Ti, which initiates interdiffusion and acts as a trigger for SHS ignition. The formation of Ti₅Si₃ appears to occur by the direct solid state reaction of β-Ti and Si.]]> Sat 24 Mar 2018 07:20:26 AEDT ]]> https://ogma.newcastle.edu.au/vital/access/ /manager/Repository/uon:3435 Sat 24 Mar 2018 07:20:25 AEDT ]]> https://ogma.newcastle.edu.au/vital/access/ /manager/Repository/uon:3167 2 μm), 237–245 Ma for the <2 μm fraction, 218 Ma for the <0.4 μm fraction and 196 Ma for the <0.1 μm fraction have been obtained from siltstones within and outside the damage zone. We believe the younger ages of 196–237 Ma indicate the time at which diagenetic illite–smectite formed and the 122–150 Ma dates from the <2 μm fraction represent the maximum age of gouge formation. The younger ages are thought to reflect the last slip event occurring on the faults, which is related to the rifting and dispersal of the eastern margin of the Australian continent.]]> Sat 24 Mar 2018 07:18:10 AEDT ]]>