...
机译:9°50'N东太平洋上升带的热液羽流中溶解的颗粒有机碳
School of Ocean and Earth Science, National Oceanography Centre, Southampton SO14 3ZH, UK;
School of Ocean and Earth Science, National Oceanography Centre, Southampton SO14 3ZH, UK;
National Environment Research Council, National Oceanography Centre, Southampton SO14 3ZH, UK;
Universite Pierre et Marie Curie—Paris 6, CNRS UPMC FRE3350 LECOB, 66650 Banyuls-sur-mer, France;
University of New Hampshire, Durham, NH 03824, USA;
University of New Hampshire, Durham, NH 03824, USA;
Woods Hole Oceanographic Institution, Woods Hole, MA 02543, USA ,Universite Europeenne de Bretagne, European Institute for Marine Studies IUEM, Technopole Brest-Iroise, 29280 Plouzane, France;
University of New Hampshire, Durham, NH 03824, USA;
Woods Hole Oceanographic Institution, Woods Hole, MA 02543, USA;
hydrothermal; dissolved organic carbon; particulate organic carbon; east pacific rise;
机译:东太平洋上升9°45'N的热液羽流中溶解的颗粒状Fe:太平洋羽流中缓慢的Fe(II)氧化动力学
机译:赤道中部太平洋中溶解的微粒Th-230-Th-232:东太平洋上升热液羽流的远场运输证据
机译:来自东太平洋海拔90'N的东太平洋深海水热通气流体中的溶解有机碳化合物
机译:12°50′N和11°30′N附近东太平洋上升快速段大量热液矿床的地质
机译:东北太平洋扩散脊和相关沉积物上的热液羽流:北太平洋11度和北21度附近的东太平洋上升带,Explorer Ridge和J. Tuzo Wilson Seamounts。
机译:来自中国巡航的水热羽流量检测数据集到赤道东太平洋崛起
机译:来自东太平洋深海水热通风液中的溶解有机碳化合物在9°50'N的9°