Granitic plutons (the Dolina Będkowska valley and Pilica area) were found in a few boreholes in the Małopolska Block (MB). These granitic rocks may represent apical parts (apophyses) of a great magmatic bodies (batholiths) located in deeper level of the Ediacaran/Paleozoic basement. They are described as ‘stitching intrusions’, generated during/after collision in Carboniferous/Permian period (~300 Ma) between the Upper Silesian Block (USB) and the Małopolska Block (MB). These rocks are fresh, unaltered granodiorites that are pale grey in colour. They have holocrystalline, medium- to coarse-grained structure and massive texture. For the first time, several mafic microgranular enclaves (MME), varying in size and colour, were found in the gran...
Tonalitic, granodioritic and monzogranitic enclaves occur in the Hercynian peraluminous porphyritic ...
Post-collisional magmatic intrusions and their mafic microgranular enclaves (MMEs) can provide si...
Four mid- to late Devonian peraluminous granitoid intrusions in the Meguma Zone of southwestern Nova...
The Devonian–early Carboniferous (354.1±3.5 Ma: conventional zircon U–Pb age) Sázava intrusion (biot...
The Devonian–early Carboniferous (354.1±3.5 Ma: conventional zircon U–Pb age) Sázava intrusion (biot...
Enclaves are typical objects found commonly in the granitoid plutons. Different genetical types of ...
The Jawornik granitoids intrude, in vein-like form, a sequence of a polymetamorphic metavolcanic and...
Sparse microgranitoid enclaves (MGE) in the leucocratic I-type Looanga monzogranite near Bendemeer, ...
Variscan granitoids occur in the southeastern part of the Tisza Mega Unit of Hungary. The presence o...
The enclave swarm of Pomarinho is located in the SW edge of Évora granitoid, in the SW sector of the...
The Agacoren Intrusive Suite is exposed as a large intrusive body over ∼500 km2 east of Lake Tuz in ...
Monsildale Granodiorite is a small (36 km2 ) Permo-Triassic intra-terrane composite pluton intruding...
The Ghohroud granitoids (GG), containing mafic microgranular enclaves (MMEs) are located in the cent...
The plutonic complex of Cima d'Asta is an example of hybrid magmatism, due to the interaction of maf...
The enclave swarm of Pomarinho is located in the SW edge of Évora granitoid [1], in the SW sector of...
Tonalitic, granodioritic and monzogranitic enclaves occur in the Hercynian peraluminous porphyritic ...
Post-collisional magmatic intrusions and their mafic microgranular enclaves (MMEs) can provide si...
Four mid- to late Devonian peraluminous granitoid intrusions in the Meguma Zone of southwestern Nova...
The Devonian–early Carboniferous (354.1±3.5 Ma: conventional zircon U–Pb age) Sázava intrusion (biot...
The Devonian–early Carboniferous (354.1±3.5 Ma: conventional zircon U–Pb age) Sázava intrusion (biot...
Enclaves are typical objects found commonly in the granitoid plutons. Different genetical types of ...
The Jawornik granitoids intrude, in vein-like form, a sequence of a polymetamorphic metavolcanic and...
Sparse microgranitoid enclaves (MGE) in the leucocratic I-type Looanga monzogranite near Bendemeer, ...
Variscan granitoids occur in the southeastern part of the Tisza Mega Unit of Hungary. The presence o...
The enclave swarm of Pomarinho is located in the SW edge of Évora granitoid, in the SW sector of the...
The Agacoren Intrusive Suite is exposed as a large intrusive body over ∼500 km2 east of Lake Tuz in ...
Monsildale Granodiorite is a small (36 km2 ) Permo-Triassic intra-terrane composite pluton intruding...
The Ghohroud granitoids (GG), containing mafic microgranular enclaves (MMEs) are located in the cent...
The plutonic complex of Cima d'Asta is an example of hybrid magmatism, due to the interaction of maf...
The enclave swarm of Pomarinho is located in the SW edge of Évora granitoid [1], in the SW sector of...
Tonalitic, granodioritic and monzogranitic enclaves occur in the Hercynian peraluminous porphyritic ...
Post-collisional magmatic intrusions and their mafic microgranular enclaves (MMEs) can provide si...
Four mid- to late Devonian peraluminous granitoid intrusions in the Meguma Zone of southwestern Nova...