On the origin of the Southern Permian Basin, Central Europe

Wees, J.D.A.M. van; Stephenson, Randell; Ziegler, Peter A.; Bayer, U.; McCann, Tom; Dadlez, Ryszard; Gaupp, Reinhard; Narkiewicz, Marek; Bitzer, Frank; Scheck, M.

doi:10.1016/s0264-8172(99)00052-5

Cited by 261 publications

(156 citation statements)

References 28 publications

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“…a mantle plume or, possibly, several plumes). In detail, however, it is likely that uplift was induced by a complex combination of wrench-related lithospheric deformation, magmatic inflation of the lithosphere and thermal erosion of the base of the lithosphere (van Wees et al 2000).…”

mentioning

confidence: 99%

Permo-Carboniferous magmatism and rifting in Europe: introduction

et al. 2004

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mentioning

confidence: 99%

Permo-Carboniferous magmatism and rifting in Europe: introduction

et al. 2004

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“…The post -Variscan cover of Perm ian-Me so zoic for ma tions was likely de posited over the Fore-Sudetic Block, but was eroded dur ing Lara mide move ments. The Perm ian to Early Tri as sic extensional stage is con sis tent with the Late Perm ian-Early Ju ras sic tec tonic sub si dence curves im ply ing that Perm ian and Tri as sic rift ing pre dom i nantly mod i fied the con fig u ra tion of the South ern Perm ian Ba sin (van Wees et al, 2000).…”

Section: Geological Backgroundmentioning

confidence: 55%

“…Dur ing the Perm ian, the area of SW Po land be longed to the South ern Perm ian Ba sin which was formed at the tran si tion from the Carbon if er ous to Early Perm ian as a re sult of sub sidence by rift ing (van Wees et al, 2000). A num ber of sub-de pres sions sep a rated by ridges de veloped, in clud ing the Wolsztyn-Pogorzela High which sep a rated the Zielona Góra Ba sin from the Variscan Fore land (Kiersnowski et al, 2010).…”

Section: Geological Backgroundmentioning

confidence: 99%

Controls on the distribution of rare earth elements in the Kupferschiefer series of SW Poland

Oszczepalski¹,

Chmielewski²,

Mikulski³

2016

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1 Pol ish Geo log i cal In sti tute -Na tional Re search In sti tute, Rakowiecka 4, 00-975 Warszawa, Po land Oszczepalski, S., Chmielewski, A., Mikulski, S.Z., 2016. Con trols on the dis tri bu tion of rare earth el e ments in the Kupferschiefer se ries of SW Po land. Geo log i cal Quar terly, 60 (4): 811-826, doi: 10.7306/gq.1325 This study deals with the spa tial dis tri bu tion and the PAAS-nor mal ized pat terns of rare earth el e ments (REE) stud ied by ICP-MS in the Kupferschiefer se ries of SW Po land. The most char ac ter is tic fea ture is a pro gres sive en rich ment in REE content (in clud ing Y and Sc) out ward from the rocks with py ritic and Pb-Zn min er al isa tion, across the rocks with cop per min er alisa tion, to wards the ox i dized (Rote Fäule) ar eas. The same trend can also be ob served with re spect to LREE, MREE and HREE. Whereas REE dis tri bu tion di a grams for shales with py rite and Pb-Zn min er al isa tion are al most flat, di a grams for shales with he ma tite and cop per min er al isa tion are con vex-up ward and the stron gest con vex ity is at trib uted to the tran si tion from hematitic al ter ation to cop per-rich rocks. REE dis tri bu tion di a grams nor mal ized to PAAS show strong MREE en richment rel a tive to LREE and HREE, which is typ i cally the high est in the he ma tite zone, lower in shale with cop per min er al isation, and the low est in shales with Pb-Zn and py rite min er al isa tion. The sys tem atic in crease in the con cen tra tion of REE to wards the Rote Fäule, and the strong en rich ment in MREE in the tran si tion zone are in dic a tive of vari able in ten sity of leaching and for ma tion of the REE en rich ments (in clud ing MREE) by MREE>HREE>LREE flu ids, as ev i denced by the MREE-enriched sig na tures. Over print ing of sec ond ary en rich ments over the orig i nal REE pat tern due to re dis tri bu tion along the path ways of ex pand ing flu ids are pos tu lated to ac count for the ap par ent dif fer ences in the dis tri bu tion and con cen tra tion of REE (in clud ing the MREE-en riched trend) be tween the ox i dized rocks, cop per-bear ing rocks, and re duced lithologies bar ren in cop per.

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“…Сум-марная их мощность невелика: до 1,5-2 км наблюдаются в Иберии (северо-восток Испании) [Arche, Lopez-Gomez, 1996;Vargas et al, 2009], при этом на разрезах фиксируются как минимум двукратные размывы [Bourquin et al, 2007]. Происхождение этих бассейнов проблематично с геодинамической точ-ки зрения, так как последний период тектономагматической активизации в регионе, с которой можно очевидным образом связать рифтогенез, завер-шился за 20 млн лет до того в ранней перми (примерно 285 млн лет) [Циглер, 1981;Van Wees et al, 2000].…”

unclassified

“…7. Сравнение кривых тектонического по-гружения для пермско-триасовых бассейнов За-падной Европы: а -участка Молина де Арагон в Иберии [Vargas et al, 2009]; б -скважины в преде-лах Южно-пермского бассейна северо-западной части Европы [van Wees et al, 2000]; в -впадины Эбро в настоящей статье (1, 2 -этапы пассивного и активного рифтогенеза соответственно, 3 -пе-риоды тектонически неопределенного развития бассейна в связи с размывом отложений [Vargas et al, 2009]). ми активного рифтинга RI и RII, когда для второго (позднепермского) преду-сматривается варьирование режима в виде трех фаз с различными индексами утонения коры (см.…”

unclassified

Vertical tectonic movements and sedimentary filling of basins during syn-rift and post-rift stages of lithosphere development

Gonchar¹

2017

Geofizicheskiy Zhurnal

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On the origin of the Southern Permian Basin, Central Europe

Cited by 261 publications

References 28 publications

Permo-Carboniferous magmatism and rifting in Europe: introduction

Permo-Carboniferous magmatism and rifting in Europe: introduction

Controls on the distribution of rare earth elements in the Kupferschiefer series of SW Poland

Vertical tectonic movements and sedimentary filling of basins during syn-rift and post-rift stages of lithosphere development

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