isvav_result

publication_year

occurrences__organization__code

solver__id__sc2

result_type__code

Type of result according to the RIV classification. Czech version is available <a href="https://www.vyzkum.cz/FrontClanek.aspx?idsekce=1395" target="_blank" >here</a>.

language__code

Jazyk výsledku udáva původní jazyk, ve kterém byl daný výsledek vytvořen. Kompletní seznam jazyků ve kterém je možno výsledek do RIV předložit je <a href="https://www.vyzkum.cz/FrontClanek.aspx?idsekce=1397" target="_blank" >zde</a>.

cep__code

ford__code

_group_id67

occurrences__funder__code

Data supplier is the R&D aid provider who supported this result.

project__programme__code

x_range_count_solvers

project__id

What are you looking for?

Quick search

Smart search

Filters

Simultaneous free flow and forcefully driven movement of magma in lamprophyre dykes as indicated by magnetic anisotropy: Case study from the Central Bohemian Dyke Swarm, Czech Republic

Anisotropy of out-of-phase magnetic susceptibility as a potential tool for distinguishing geologically and physically controlled inverse magnetic fabrics in volcanic dykes

Magma chamber construction during crustal thickening and subsequent exhumation: An example of interplay between magmatic and tectonic processes from the Central Bohemian Batholith (Bohemian Massif)

Structural study, AMS and thermorheological modelling of syn-tectonic emplacement of mingled tonalitic and mafic magmas during oblique transpression: an example from the SE margin of the Teplá-Barrandian Zone

Eastern Margin of the Tuolumne Intrusive Suite (Sierra Nevada Batholith): Magmatic fabrics, Internal structures, Host Rocks Deformation and Emplacement Models in an Continental Island Arc Magma Chamber

A plate-kinematic model for assembly of the Bohemian Massif constrained by structural relationships around granitoid plutons

Identifying plutons associated with long-lived volcanism by thermal modeling of contact metamorphic aureoles

Reply to the comments on Magmatic history and geophysical signature of a post-collisional intrusive center emplaced near a crustal-scale shear zone: the Plechy´ granite pluton (Moldanubian batholith, Bohemian Massif)

Magnetic fabric and emplacement of dykes of lamprophyres and related rocks of the Central Bohemian Dyke Swarm (Central European Variscides)

Ultrahigh-temperature granites and a curious thermal eye in the post-collisional South Bohemian batholith of the Variscan orogenic belt (Europe)