Structural and anisotropy of magnetic susceptibility records of granitoid sheets emplacement during growth of a continental gneiss dome (Central Sudetes, European Variscan Belt)

Abstract

[1] Granitoid magmatic sheets emplaced syntectonically during growth of the Orlica-Śnieżnik mantled gneiss dome (Central Sudetes, European Variscan belt) were examined by means of structural geology, quartz, and anisotropy of magnetic susceptibility (AMS) fabric studies. Magmatic emplacement was localized along the eastern transpressive margin of the high metamorphic core and below the low-grade detached mantle rimming the southern margin of the dome. In the first area, the magmatic sheets were emplaced parallel to the dilated subhorizontal foliation of an anisotropic pre-orogenic block. The resulting melt-host rock multilayer localized the transpressive zone along which the bulk of magma was emplaced. The AMS study shows an across-strike fabric zonation underlying a strongly transpressive solid-state deformation in the hanging-wall, magmatic subhorizontal fabric in the foot-wall and a transitional fabric in the center of the intrusion. In contrast, along the southern dome margin, magmatic sheets intruded along steep foliations of weakly metamorphic mantle rocks, and are affected by recumbent folding and subhorizontal shearing. The bulk of the sheets present a shallow-dipping magmatic foliation and an along-strike magmatic lineation. The variations of the quartz and magnetic fabrics are attributed to superimposition of pure shear-dominated ductile thinning followed by simple shear-dominated detachment onto the original steep fabric. AMS modeling confirms the role of variation of orientation of pre-intrusive anisotropy during progressive deformation on the resulting fabric pattern and helps explaining observed variations in fabric orientations and symmetries. This study highlights contrasting mechanical behavior of syntectonically emplaced magmas in different parts of a growing crustal-scale mantled gneiss dome.

Interactions between plutonism and detachments during metamorphic core complex formation, Serifos Island (Cyclades, Greece)

“…The deepest parts of the intrusion with magmatic inclusions have been dragged southwestward along southwest dipping shear zones, while the magma was still unconsolidated and ultimately sheared below the WCDS. A similar geometry was inferred for other plutons emplaced into zones affected by noncoaxial shearing [ Bouillin et al , ; Acocella and Rossetti , ; Kratinová et al , ; Denèle et al , ; Lehmann et al , ; Laurent et al , ] and also modeled by Schulmann and Ježek [].…”

Mechanical anisotropies and mechanisms of mafic magma ascent in the middle continental crust: The Sondalo magmatic system (N Italy)

“…On the grain scale, the transposition occurs without kinking or folding of the previous fabric indicating that crystals were individually rotated while being still separated by a liquid fraction (crystal mush). The transposition process and its impact on the AMS ellipsoid and parameters should be similar to that described and modelled by Lehmann et al (2013). These authors show that the transposition of a magmatic fabric leads to a strong c-axis orientation of elongated minerals (e.g.…”

Time‐scale of deformation and intertectonic phases revealed byP–T–D–trelationships in the orogenic middle crust of the Orlica‐Śnieżnik Dome, Polish/Czech Central Sudetes

“…The OSD core comprises synforms of metasedimentary rocks (so‐called Stronie and Młynowiec formations), surrounded by antiforms of orthogneiss (Śnieżnik and Gierałtów types) with small bodies of eclogite and high‐ P (HP) granulite. Elongated sheets of syntectonic granitoid are found within the OSD mantle and locally within the OSD core (Lehmann et al ., ; Fig. ).…”