000034017 001__ 34017
000034017 041__ $$aEnglish
000034017 100__ $$aBenn, D. I.
000034017 245__ $$aThe Role of the Indian Summer Monsoon and the Mid-Latitude Westerlies in Himalayan Glaciation: Review and Speculative Discussion
000034017 260__ $$c1998
000034017 300__ $$a353-363
000034017 511__ $$aIndus, IndusARTICLES
000034017 520__ $$aNew dares for late Quaternary glaciations in the Himalayas show that,\nduring the last glacial cycle, glaciations were not synchronous throughout\nthe region. Rather, in some areas glaciers reached their maxima at\nthe global glacial maximum of e. 18-20 ka sp, whereas in others glaciers\nwere most extensive at c. 60-30 ka sp. Comparison of these data with\npalaeoclimatic records from adjacent regions suggest that, on millennial\ntimescales, Himalayan glacier fluctuations are controlled by variations\nin both the South Asian monsoon and the mid-latitude westerlies.
000034017 700__ $$aOwen, L. A.
000034017 773__ $$a10.1144/gsjgs.155.2.0353
000034017 773__ $$pJournal of the Geological Society
000034017 773__ $$v155 (2)
000034017 8564_ $$uhttp://jgs.lyellcollection.org/lookup/doi/10.1144/gsjgs.155.2.0353$$yExternal link
000034017 980__ $$aARTICLE