The Margins of Laurussia in Central and Southeast Europe and Southwest Asia

KALVODA, Jiří a Ondřej BÁBEK. The Margins of Laurussia in Central and Southeast Europe and Southwest Asia. Gondwana Research. Elsevier, 2010, roč. 17, 2-3, s. 526-545, 19 s. ISSN 1342-937X.

Základní údaje

• Originální název: The Margins of Laurussia in Central and Southeast Europe and Southwest Asia
• Název česky: The Margins of Laurussia in Central and Southeast Europe and Southwest Asia
• Autoři: KALVODA, Jiří (203 Česká republika, garant, domácí) a Ondřej BÁBEK (203 Česká republika, domácí).
• Vydání: Gondwana Research, Elsevier, 2010, 1342-937X.

Další údaje

• Originální jazyk: angličtina
• Typ výsledku: Článek v odborném periodiku
• Obor: 10500 1.5. Earth and related environmental sciences
• Stát vydavatele: Nizozemské království
• Utajení: není předmětem státního či obchodního tajemství
• Impakt faktor: Impact factor: 5.503
• Kód RIV: RIV/00216224:14310/10:00047656
• Organizační jednotka: Přírodovědecká fakulta
• UT WoS: 000274911600024
• Klíčová slova česky: Laurussia; Peri-Gondwana; Rheic suture
• Klíčová slova anglicky: Laurussia; Peri-Gondwana; Rheic suture
• Štítky: Gondwana, Laurussia, tectonostratigraphy, Variscides

Anotace

The continuation of the Laurussian margin into central and southeast Europe and southwest Asia is defined by the Rheic suture, which becomes harder to trace to the southeast because of complex post-Variscan strike-slip displacements and tectonic stacking linked to the Cimmerian and Alpine cycles. The uncertain extent of the Neoproterozoic Baikalian orogeny fringing Baltica, ambiguous early Paleozoic paleobiogeographic data, and strike-slip activity complicate the distinction of the Tornquist suture from the Transeuropean Suture Zone. There is growing evidence for the incorporation of the Brunovistulian, Malopolska and West Moesian terranes into the late Neoproterozoic–Cambrian Baltican margin. The Istanbul–Zonguldak terrane, along with the Bítesh and East Moesia terranes, may have been part of the Avalonian terrane assemblage, although an Arabian–Nubian Shield or Baltica provenance cannot be excluded. The terranes of the Armorica terrane assemblage bordering the Rheic suture include the Outer Carpathian, Tatra, Getic and Balkan terranes in southeast Europe and Sakarya and the Anatolide–Tauride terrane in Turkey. Further east, the Rheic suture may be present in the Caucasus, in all probability between the Greater Caucasus and the Scythian Platform or, alternatively, between the Greater Caucasus and Transcaucasia. Alborz, in northern Iran, is interpreted as a distal part of Transcaucasia. The location of the Rheic suture in the southeast part of the Turan domain of Central Asia is poorly constrained.

Anotace česky

The continuation of the Laurussian margin into central and southeast Europe and southwest Asia is defined by the Rheic suture, which becomes harder to trace to the southeast because of complex post-Variscan strike-slip displacements and tectonic stacking linked to the Cimmerian and Alpine cycles. The uncertain extent of the Neoproterozoic Baikalian orogeny fringing Baltica, ambiguous early Paleozoic paleobiogeographic data, and strike-slip activity complicate the distinction of the Tornquist suture from the Transeuropean Suture Zone. There is growing evidence for the incorporation of the Brunovistulian, Malopolska and West Moesian terranes into the late Neoproterozoic–Cambrian Baltican margin. The Istanbul–Zonguldak terrane, along with the Bítesh and East Moesia terranes, may have been part of the Avalonian terrane assemblage, although an Arabian–Nubian Shield or Baltica provenance cannot be excluded. The terranes of the Armorica terrane assemblage bordering the Rheic suture include the Outer Carpathian, Tatra, Getic and Balkan terranes in southeast Europe and Sakarya and the Anatolide–Tauride terrane in Turkey. Further east, the Rheic suture may be present in the Caucasus, in all probability between the Greater Caucasus and the Scythian Platform or, alternatively, between the Greater Caucasus and Transcaucasia. Alborz, in northern Iran, is interpreted as a distal part of Transcaucasia. The location of the Rheic suture in the southeast part of the Turan domain of Central Asia is poorly constrained.

Návaznosti

• GA205/08/0182, projekt VaV: Název: Vysoce rozlišující stratigrafie hraničního intervalu tournai a visé

Investor: Grantová agentura ČR, Vysoce rozlišující stratigrafie hraničního intervalu tournai a visé

• MSM0021622412, záměr: Název: Interakce mezi chemickými látkami, prostředím a biologickými systémy a jejich důsledky na globální, regionální a lokální úrovni (INCHEMBIOL) (Akronym: INCHEMBIOL)

Investor: Ministerstvo školství, mládeže a tělovýchovy ČR, Interakce mezi chemickými látkami, prostředím a biologickými systémy a jejich důsledky na globální , regionální a lokální úrovni