4.4 Article

Tertiary alkaline Roztoky Intrusive Complex, Ceske stredohori Mts., Czech Republic: petrogenetic characteristics

Journal

INTERNATIONAL JOURNAL OF EARTH SCIENCES
Volume 103, Issue 5, Pages 1233-1262

Publisher

SPRINGER
DOI: 10.1007/s00531-013-0948-7

Keywords

Bohemian Massif; Cenozoic; Continental rift; Roztoky Intrusive Complex; Alkaline intrusions; Geochemistry

Funding

  1. Grant Agency of the Academy of Sciences of the Czech Republic [IAA300130902]
  2. Institute of Geology, v. v. i. [RVO67985831]
  3. Ministry of Education (Charles University) [MSM 0021620855]

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The Ceske stredohori Mts. is the dominant volcanic center of the Ohre (Eger) rift zone. It hosts the Roztoky Intrusive Complex (RIC), which is made up of a caldera vent and intrusions of 33-28-Ma-old hypabyssal bodies of essexite-monzodiorite-sodalite syenite series accompanied by a radially oriented 30-25-Ma-old dike swarm comprising about 1,000 dikes. The hypabyssal rocks are mildly alkaline mostly foid-bearing types of mafic to intermediate compositions. The dike swarm consists of chemically mildly alkaline and rare strongly alkaline rocks (tinguaites). The geochemical signatures of the mildly alkaline hypabyssal and associated dike rocks of the RIC are consistent with HIMU mantle sources and contributions from lithospheric mantle. The compositional variations of essexite and monzodiorite can be best explained by fractional crystallization of parent magma without significant contributions of crustal material. On the other hand, the composition of monzosyenite, leuco-monzodiorite and sodalite syenite reflects fractional crystallization coupled with variable degrees of crustal assimilation. It is suggested that the parent magmas in the Ohre rift were produced by an adiabatic decompression melting of ambient upper mantle in response to lithospheric extension associated with the Alpine Orogeny.

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