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| 1 | Newmark displacement model for landslides induced by the 2013 Ms 7.0 Lushan earthquake, China显示文摘 | Renmao YUAN Qinghai DENG Dickson CUNNINGHAM Zhujun HAN Dongli ZHANG Bingliang ZHANG | 2016 | Frontiers of Earth Science2016，10，4： | 7 |
| 2 | Capecitabine and mitomycin C as third-line therapy for patients with metastatic colorectal cancer resistant to fluorouracil and irinotecan显示文摘 | Chong G Dickson JL Cunningham D | 2005 | Br J Cancer2005，93，5： | 1 |
| 3 | A new terrane subdivision for Mongolia: implications for the Phanerozoic crustal growth of Central Asia显示文摘 | Badarch G Dickson Cunningham W Windley B F | 2002 | Journal of Asian Earth Sciences2002，21，1： | 1 |
| 4 | Capeeitabine and mitomycin C as Ihird-line therapy 1br patients with metastatic colorectal cancer resistant to fluorouracil and irinotecan显示文摘 | Chong G Dickson Jl Cunningham D | 2005 | Br J Cancer2005，93，5： | 1 |
| 5 | Systemic treatment of gastric cancer显示文摘 | Dickson James LB Cunningham D | 2004 | European Journal of Gastroenterology & Hepatology2004，16，3： | 1 |
| 6 | Mountain building processes in intracontinental oblique deformation belts: Lessons from the Gobi Corridor, Central Asia显示文摘 | Dickson Cunningham | 2013 | Journal of Structural Geology2013，，： | 1 |
| 7 | Systemic treatment of gastric cancer显示文摘 | Dickson JL Cunningham D | 2004 | Eur J Gastroenterol Hepatol2004，16，3： | 1 |
| 8 | Systemic treatment of gastric cancer 显示文摘 | Dickson JLB Cunningham D | 2004 | Eur J Gastroenterol Hepatol2004，16，2： | 1 |
| 9 | Capecitabine and mitomycin C as third-line therapy for patients with metastatic colorectal cancer resistant to fluorouracil and irinotecan显示文摘 | Chong G Dickson JL Cunningham D | 2005 | Br J Cancer2005，93，5： | 1 |
| 10 | Systemic treatment of gastric cancer显示文摘 | Dickson JL Cunningham D | 2004 | Eur J Gastroenterol Hepatol2004，16，3： | 1 |
| 11 | Triassic to Cenozoic multi-stage intra-plate deformation focused near the Bogd Fault system,Gobi Altai,Mongolia显示文摘The Gobi Altai region of southern Mongolia has been in the Eurasian plate interior since the midMesozoic,yet has experienced episodic phases of deformation since that time.In this paper,we document field evidence to characterize and date the intra-plate tectonic history of the Gobi Altai region from the Triassic to the present.To this end,we provide detailed mapping of the structure and stratigraphy of the eastern flanks of Mt.Ih Bogd that contains the widest variety of rock-time units in the area.We carry out geochronological analysis of basaltic lavas and basement granite in the area.We demonstrate that a crystalline basement with a 502 ± 8 Ma granitoid(U/Pb) underwent two phases of basin formation in the Mesozoic.which we date with new ^(40)Ar/^(39)Ar lava ages of 218.5 ± 1.5,123.2 ± 0.7 and 124.8 ± 1.2 Ma,respectively.Both phases are linked to deposition of fluvio-lacustrine sediments and trap-like basaltic volcanics,with cumulative thicknesses of 1000-1500 m.Both basins were likely north-facing half-grabens that developed under ~ N-S extension,but were subsequently overthrusted by Paleozoic and older crystalline basement during a less well constrained,but likely mid-Cretaceous phase of N-S shortening and basin inversion.Our results are consistent with recent seismic imaging of rift basins ~ 100 km to the NE of the study area where a similar history was reconstructed.The multiple phases of intra-plate deformation appear to have parallel structural trends,most likely due to reactivated Paleozoic basement structures created during the original terrane amalgamation of the Central Asian Orogenic Belt continental crust.This strong basement heterogeneity may predispose it to reactivation,and make it sensitive to changes in the overall stress field of the Eurasian plate driven by forces at its margins and base.Detailed study of Mongolia's multi-stage tectonic history may thus provide a key proxy for the long-term dynamics of the Eurasian plate.In addition,the repeated reactivation of the Gobi Altai region during the last 200 My supports the contention that non-cratonized continental interior regions composed of Phanerozoic terrane collages are particularly susceptible to fault reactivation,much more than older cratonized continental crust. | Douwe J.J.van Hinsbergen Dickson Cunningham Gijsbert B.Straathof Morgan Ganerod Bart W.H.Hendriks Arjan H.Dijkstra | 2015 | Geoscience Frontiers2015，6，5： | 0 |
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