@article{Lâm_2011, title={VÀI NÉT VỀ ĐỊA CHẤT - ĐỊA MẠO BÁN ĐẢO BARTON VÀ WEIVER, ĐẢO KING GEORGE, NAM CỰC}, volume={33}, url={https://vjs.ac.vn/index.php/jse/article/view/352}, DOI={10.15625/0866-7187/33/3/352}, abstractNote={<p><strong>Some geological and geomorphological features of the Barton and Weiver peninsula, King George Island, Antarctica</strong></p> <p>Barton and Weiver peninsula, King George Island situated at periphery of Antarctica, where many scientific research stations have been set up. Gently dipping to the south and southwest, Cretaceuos-Paleogene volcaniclastic of the Sejong Formation is well spread on this peninsula with thickness about 100m. The Formation composes of 5 facies: 1/ disorganised, matrix-supported conglomerate; 2/ disorganised, clast-supported conglomerate; 3/ stratified, clast supported conglomerate; 4/ thin-bedded sandstone and 5/ tuff lapili. Quaternary deposits are moraine, tills on low-lying hills and gravels, cobbles, on the recent marine terrace or beach.</p> <p>Intrusive rocks in this area are granodiorite, diorite, gabbro and quartz monzodiorite that intruded the Sejong Formation and basaltic andesite. Effusive rocks are most spread in Barton and Wiever peninsula; consist of basalts and basaltic andesite.</p> <p>In study area, glacial relief is very common, consists of low-lying hills (150-200m height) and cliffs. There are recent marine terraces (2-3m height) and beach situated around peninsula, covered by very course deposits.</p> <p> </p>}, number={3}, journal={Vietnam Journal of Earth Sciences}, author={Lâm, Doãn Đình}, year={2011}, month={Dec.}, pages={436–442} }