机译:俄罗斯平原莫斯科冰川界限内的两方沉积物中的土壤:沉积环境,成岩作用,古地貌意义
Lomonosov Moscow State Univ, Fac Soil Sci, GSP 1,1-12 Leninskie Gory, Moscow 119991, Russia|Russian Acad Sci, Inst Geog, Staromonetniy Pereulok 29, Moscow 119017, Russia;
Russian Acad Sci, Dokuchaev Soil Sci Inst, Pyzhevsky Lane 7-2, Moscow 109017, Russia|Russian Acad Sci, Inst Geog, Staromonetniy Pereulok 29, Moscow 119017, Russia;
Russian Acad Sci, Dokuchaev Soil Sci Inst, Pyzhevsky Lane 7-2, Moscow 109017, Russia;
St Petersburg State Univ, Inst Earth Sci, Univ Skaya Nab 7-9, St Petersburg 199034, Russia;
Univ Wurzburg, Inst Geog & Geol, D-97074 Wurzburg, Germany;
Lomonosov Moscow State Univ, Fac Soil Sci, GSP 1,1-12 Leninskie Gory, Moscow 119991, Russia;
Moscow (Saalian) cryochrone; Basal till; Bipartite sediments; Soil evolution; Retisol; Russian Plain;
机译:俄罗斯平原中部和东部的中更新世成岩作用与环境
机译:俄罗斯平原冰川沉积物中的粗粉化作用及其成因
机译:“在欧洲俄罗斯内俄罗斯平原的森林草原景观带中,地形特征和景观连通性对小型农业流域的沉积物再分配的影响”勘误[Geomorphology 327(2019)230-247]
机译:不同指标在近几十年中俄罗斯平原中动态土壤侵蚀率评估的应用
机译:俄罗斯平原东南部地区河流河流域内的当代侵蚀和悬浮沉积物产量:以撒玛拉流域为例