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机译:沿活跃的冈瓦纳北部边缘进行的长期卡多马岩浆活动:波西米亚地块东部的布鲁诺维苏利地区的U-Pb锆石和Sr-Nd同位素证据
Czech Geol Survey, Klarov 3, Prague 11821 1, Czech Republic;
Czech Geol Survey, Klarov 3, Prague 11821 1, Czech Republic|Charles Univ Prague, Fac Sci, Inst Petrol & Struct Geol, Albertov 6, Prague 12843 2, Czech Republic;
Czech Geol Survey, Klarov 3, Prague 11821 1, Czech Republic;
CAS, Inst Geol, Vvi, Rozvojova 269, Prague 16500 6, Czech Republic;
Czech Geol Survey, Klarov 3, Prague 11821 1, Czech Republic|Univ Tromso, Dept Geosci, Postboks 6050, N-9037 Tromso, Norway;
CAS, Inst Geophys, Vvi, Bocni 2-1401, Prague 14131 4, Czech Republic;
Czech Geol Survey, Klarov 3, Prague 11821 1, Czech Republic;
Cadomian magmatic arc; Brunovistulian Domain; Bohemian Massif; Gondwana margin; U-Pb geochronology; Geochemistry;
机译:布尔诺岩床:洞悉波希米亚地块东缘的Cadomian Brunovistulian单元的岩浆和变质作用演化
机译:波西米亚地块的Teplá-Barrandian单元中的新元古代至早期的寒武纪方格式混杂岩:冈瓦纳Cadomian活动带沿现代增生过程的证据?
机译:比利牛斯山脉东部卡多期和奥陶纪早期岩浆活动的U-Pb锆石年龄(SHRIMP):对冈瓦纳北部北部瓦里斯坎前演化的新见解
机译:沿冈瓦纳北部边缘活跃的卡多米亚岩浆活动:来自波希米亚东部地区Brunovistulian域的U-pb锆石和sr-Nd同位素证据