@article{2-s2.0-33747198786,

title = {Magmatism and metamorphism of the Kraków-Lubliniec Tectonic zone as a clue to the occurrence of polymetallic deposits [Magmatyzm i metamorfizm strefy tektonicznej Kraków-Lubliniec jako przesłanki wystepowania złóżpolimetalicznych]},

author = { M. Truszel and Ł. Karwowski and K. Lasoń and J. Markiewicz and J. Żaba},

url = {https://www.scopus.com/inward/record.uri?eid=2-s2.0-33747198786&partnerID=40&md5=0f2b063385838e87779a3fde21135def},

issn = {02086603},

year  = {2006},

date = {2006-01-01},

journal = {Biuletyn - Panstwowego Instytutu Geologicznego},

number = {418},

pages = {55-103},

abstract = {Numerous occurrences of magmatism are observed in the vicinity of Myszków, Zawiercie, Pilica, Bedkowska Valley, Kozieglowy (Myslów) and Żarki along the Kraków-Lubliniec tectonic zone which is a contact zone of the Małopolska and Upper Silesia blocks. The formation of granitoid intrusion is related to a multiphase structural evolution of the zone whose especially intensive activity took place at the end of the Silurian and Upper Carboniferous. Ore mineralization occurs both in igneous and metamorphic wall rocks (Vendian; Palaeozoic). Igneous rocks consist of a genetically different association of intrusive rocks: granitoids (mainly granodiorites; rare granites), dacites, dolerites (diabases) and gabbros. Alterations, which show regional metamorphic nature (greenschist facies), were recorded only in the Vendian complex formations, while thermal and thermal -metasomatic metamorphism, being the effect of influence of granitoid intrusion into wall rocks, affected Vendian, Ordovician, Silurian and Devonian formations. Ore contents of the rocks show direct relationship with highly concentrated metal-rich salinewaters, closely related to acid magmatism. W, Mo, Cu, Ag, K, F, Sb, Hg, Au, Pb, Ba, As, Zn, Bi and Te are elements-pathfinders which can be applied to searching for covered porphyry deposits in other parts of the region.},

note = {14},

keywords = {},

pubstate = {published},

tppubtype = {article}

}

@article{2-s2.0-0042884348,

title = {Magmatism and metamorphism of contact zone of Malopolska and Upper Silesian blocks as indicators of porphyry deposits},

author = { Ł. Karwowski and K. Lasoń and J. Markiewicz and M. Truszel},

url = {https://www.scopus.com/inward/record.uri?eid=2-s2.0-0042884348&partnerID=40&md5=caa8dfd0019034a246035838b2603dd5},

issn = {12108197},

year  = {2003},

date = {2003-01-01},

journal = {Journal of the Czech Geological Society},

volume = {48},

number = {1-2},

pages = {76-77},

abstract = {[No abstract available]},

keywords = {},

pubstate = {published},

tppubtype = {article}

}