國立高雄大學圖資館 |

Language: English

Back

The Hagendorf-Pleystein Provincethe ...

Dill, Harald G.

The Hagendorf-Pleystein Provincethe center of pegmatites in an ensialic orogen /

Record Type:	Electronic resources : Monograph/item
Title/Author:	The Hagendorf-Pleystein Provinceby Harald G. Dill.
Reminder of title:	the center of pegmatites in an ensialic orogen /
Author:	Dill, Harald G.
Published:	Cham :Springer International Publishing :2015.
Description:	xiv, 475 p. :ill., digital ;24 cm.
Contained By:	Springer eBooks
Subject:	Pegmatites.
Online resource:	http://dx.doi.org/10.1007/978-3-319-18806-5
ISBN:	9783319188065$q(electronic bk.)

The Hagendorf-Pleystein Provincethe center of pegmatites in an ensialic orogen /
Dill, Harald G.

The Hagendorf-Pleystein Provincethe center of pegmatites in an ensialic orogen /[electronic resource] :by Harald G. Dill. - Cham :Springer International Publishing :2015. - xiv, 475 p. :ill., digital ;24 cm. - Modern approaches in solid earth sciences,v.151876-1682 ;. - Modern approaches in solid earth sciences ;v.7..

Geological and geographic setting of the HPPP -- Geology and lithology of the pegmatites, aplites, dykes and granites of the HPPP -- Mineralogy of the pegmatites, aplites, dykes and granites of the HPPP -- Pegmatites and aplites of the HPPP and adjacent mineral deposits along the western edge of the BM -- The readout of the pegmatites and aplites of the HPPP in regional surveys -- The physical-chemical regime during formation and alteration of the pegmatites and aplites -- Synopsis - the evolution of pegmatites and aplites of the HPPP -- Summary and outlook on phosphate pegmatites worldwide.

This book will broaden readers' understanding of pegmatites in a special geodynamic setting, dealing with the emplacement of the Hagendorf-Pleystein Pegmatite Province (HPPP) in the Central European Variscides. This treatise illustrates the complex processes leading to the formation and partial destruction of the pegmatites, documenting the geochronological, chemical, mineralogical, geological and geomorphological / sedimentological data set. The book starts with a detailed account of the economic geology of the various pegmatites, concluding with a model of the pegmatite evolution in an ensialic orogen. The Late Paleozoic rare-element pegmatites of the HPPP, Oberpfalz-SE, Germany, rank among the largest in Europe. The biggest pegmatite of this mining district totals 4.4 million tons of ore (Hagendorf-South) The mining history of the HPPP is restricted to the 20th century, when local entrepreneurs started mining operations in search of ceramic raw materials, feldspar and quartz. Today the "Silbergrube Aplite" is still worked for feldspar. The traditional mining of pegmatitic and aplitic rocks in Central Europe, such as the Bohemian Massif, which is shared by Germany, the Czech Republic, Poland and Austria, has been focused on these industrial minerals. In addition to these commodities, lithium was mined for a period of time. But even today many of these pegmatites of calc-alkaline affiliation have not lost their appeal to mineralogists and mineral enthusiasts for their wealth of minerals that contain P, Nb, Ta, Li, Be, B, U, Th, Sc, Ti and Sn. The most favorable crustal section to bring about pegmatitic rocks of this type, encompassing pegmatoids, metapegmatites, reactivated pseudopegmatites and pegmatites sensu stricto is the ensialic orogen, exemplified by the Variscan (Hercynian) Orogen, which geodynamically connects the Paleozoic pegmatite provinces in North America and Europe. The geological history of the HPPP, however, goes much further than the Carboniferous-Permian magmatic activity, when the last structural disturbances of the Variscan orogeny affected the NE-Bavarian Basement between 450 and 330 Ma. During this time mafic magmatic rocks together with sedimentary rocks were converted to paragneisses, calcsilicates and amphibolites. During the Late Permian, the Mesozoic and the Cenozoic, the HPPP did not lie idle in geological terms; hypogene and supergene alteration continued and found its most recent expression in alluvial-fluvial "nigrine" placer deposits, which resulted from the unroofing of the pegmatites and aplites in the HPPP and can be used as a general ore guide to pegmatites.

ISBN: 9783319188065$q(electronic bk.)

Standard No.: 10.1007/978-3-319-18806-5doiSubjects--Topical Terms:

731418
Pegmatites.

LC Class. No.: QE462.P4

Dewey Class. No.: 552.3

The Hagendorf-Pleystein Provincethe center of pegmatites in an ensialic orogen /
LDR:04288nmm a2200325 a 4500 001 476756
003 DE-He213
005 20160502152533.0
006 m d
007 cr nn 008maaau
008 160526s2015 gw s 0 eng d
020 $a 9783319188065$q(electronic bk.)
020 $a 9783319188058$q(paper)
024 7 $a 10.1007/978-3-319-18806-5 $2 doi
035 $a 978-3-319-18806-5
040 $a GP $c GP
041 0 $a eng
050 4 $a QE462.P4
072 7 $a RBGK $2 bicssc
072 7 $a SCI019000 $2 bisacsh
082 0 4 $a 552.3 $2 23
090 $a QE462.P4 $b D578 2015
100 1 $a Dill, Harald G. $3 731417
245 1 4 $a The Hagendorf-Pleystein Province $h [electronic resource] : $b the center of pegmatites in an ensialic orogen / $c by Harald G. Dill.
260 $a Cham : $b Springer International Publishing : $b Imprint: Springer, $c 2015.
300 $a xiv, 475 p. : $b ill., digital ; $c 24 cm.
490 1 $a Modern approaches in solid earth sciences, $x 1876-1682 ; $v v.15
505 0 $a Geological and geographic setting of the HPPP -- Geology and lithology of the pegmatites, aplites, dykes and granites of the HPPP -- Mineralogy of the pegmatites, aplites, dykes and granites of the HPPP -- Pegmatites and aplites of the HPPP and adjacent mineral deposits along the western edge of the BM -- The readout of the pegmatites and aplites of the HPPP in regional surveys -- The physical-chemical regime during formation and alteration of the pegmatites and aplites -- Synopsis - the evolution of pegmatites and aplites of the HPPP -- Summary and outlook on phosphate pegmatites worldwide.
520 $a This book will broaden readers' understanding of pegmatites in a special geodynamic setting, dealing with the emplacement of the Hagendorf-Pleystein Pegmatite Province (HPPP) in the Central European Variscides. This treatise illustrates the complex processes leading to the formation and partial destruction of the pegmatites, documenting the geochronological, chemical, mineralogical, geological and geomorphological / sedimentological data set. The book starts with a detailed account of the economic geology of the various pegmatites, concluding with a model of the pegmatite evolution in an ensialic orogen. The Late Paleozoic rare-element pegmatites of the HPPP, Oberpfalz-SE, Germany, rank among the largest in Europe. The biggest pegmatite of this mining district totals 4.4 million tons of ore (Hagendorf-South) The mining history of the HPPP is restricted to the 20th century, when local entrepreneurs started mining operations in search of ceramic raw materials, feldspar and quartz. Today the "Silbergrube Aplite" is still worked for feldspar. The traditional mining of pegmatitic and aplitic rocks in Central Europe, such as the Bohemian Massif, which is shared by Germany, the Czech Republic, Poland and Austria, has been focused on these industrial minerals. In addition to these commodities, lithium was mined for a period of time. But even today many of these pegmatites of calc-alkaline affiliation have not lost their appeal to mineralogists and mineral enthusiasts for their wealth of minerals that contain P, Nb, Ta, Li, Be, B, U, Th, Sc, Ti and Sn. The most favorable crustal section to bring about pegmatitic rocks of this type, encompassing pegmatoids, metapegmatites, reactivated pseudopegmatites and pegmatites sensu stricto is the ensialic orogen, exemplified by the Variscan (Hercynian) Orogen, which geodynamically connects the Paleozoic pegmatite provinces in North America and Europe. The geological history of the HPPP, however, goes much further than the Carboniferous-Permian magmatic activity, when the last structural disturbances of the Variscan orogeny affected the NE-Bavarian Basement between 450 and 330 Ma. During this time mafic magmatic rocks together with sedimentary rocks were converted to paragneisses, calcsilicates and amphibolites. During the Late Permian, the Mesozoic and the Cenozoic, the HPPP did not lie idle in geological terms; hypogene and supergene alteration continued and found its most recent expression in alluvial-fluvial "nigrine" placer deposits, which resulted from the unroofing of the pegmatites and aplites in the HPPP and can be used as a general ore guide to pegmatites.
650 0 $a Pegmatites. $3 731418
650 0 $a Pegmatites $z Europe. $3 731419
650 0 $a Orogenic belts. $3 731420
650 1 4 $a Earth Sciences. $3 309702
650 2 4 $a Geochemistry. $3 196060
650 2 4 $a Mineral Resources. $3 273727
650 2 4 $a Economic Geology. $3 274135
650 2 4 $a Sedimentology. $3 196217
650 2 4 $a Geomorphology. $3 294420
710 2 $a SpringerLink (Online service) $3 273601
773 0 $t Springer eBooks
830 0 $a Modern approaches in solid earth sciences ; $v v.7. $3 676971
856 4 0 $u http://dx.doi.org/10.1007/978-3-319-18806-5
950 $a Earth and Environmental Science (Springer-11646)