• E.V. Mikhalsky
  • B.V. Belyatsky
  • S.L. Presnyakov
  • S.G. Skublov
  • V.P. Kovach
  • N.V. Rodionov
  • A.V. Antonov
  • A.K. Saltykova
  • S.A. Sergeev
© 2014 Elsevier B.V. In this paper we present new U-Pb zircon age, Sm-Nd isotopic and chemical composition data for rocks cropping out in a few isolated nunataks in Wilhelm II Land in East Antarctica, namely Mirny oasis, Mt Brown and Gaussberg volcano, which contains xenogenic crustal material. These outcrops were subjects of geological investigations during the Soviet Antarctic Expedition of 1956-1957. Our data show that this region is underlain by a uniform crust which experienced a high-grade metamorphic event at ca 980-920Ma, co-eval with the Rayner Orogeny in Kemp Land and the northern Prince Charles Mountains. Extensive indications of a ca 500Ma event in coastal areas (granitoid intrusions in Mirny oasis and inherited zircons found in Gaussberg volcano), together with the lack of indications of this age in Mt Brown, point to a concentration of ca 500Ma processes (roughly co-eval with the Prydz Orogeny) in the coastal part of Wilhelm II Land and their attenuation inland. We also determined a ca 1480Ma ag
Язык оригиналаанглийский
Страницы (с-по)171-185
ЖурналPrecambrian Research
Том258
DOI
СостояниеОпубликовано - 2015

ID: 3980418