<?xml version="1.0" encoding="UTF-8"?>
<collection xmlns="http://www.loc.gov/MARC21/slim">
 <record>
  <leader>     naa a22        4500</leader>
  <controlfield tag="001">510755313</controlfield>
  <controlfield tag="003">CHVBK</controlfield>
  <controlfield tag="005">20180411083120.0</controlfield>
  <controlfield tag="007">cr unu---uuuuu</controlfield>
  <controlfield tag="008">180411e20130301xx      s     000 0 eng  </controlfield>
  <datafield tag="024" ind1="7" ind2="0">
   <subfield code="a">10.1007/s12594-013-0044-4</subfield>
   <subfield code="2">doi</subfield>
  </datafield>
  <datafield tag="035" ind1=" " ind2=" ">
   <subfield code="a">(NATIONALLICENCE)springer-10.1007/s12594-013-0044-4</subfield>
  </datafield>
  <datafield tag="100" ind1="1" ind2=" ">
   <subfield code="a">Raiverman</subfield>
   <subfield code="D">V.</subfield>
   <subfield code="u">708 Maitri Apartment, 255 N.S.C. Bose Road, 700 047, Kolkata, India</subfield>
   <subfield code="4">aut</subfield>
  </datafield>
  <datafield tag="245" ind1="1" ind2="2">
   <subfield code="a">A brief account of the continuum from Karakoram and Himalayan ranges to foreland and ocean basins</subfield>
   <subfield code="h">[Elektronische Daten]</subfield>
   <subfield code="c">[V. Raiverman]</subfield>
  </datafield>
  <datafield tag="520" ind1="3" ind2=" ">
   <subfield code="a">Himalayan orogeny in relation to Global Tectonics is a hotly debated subject. Orogeny can result either from collision of continental plates or by an endogenic process of mantle upwelling along pre-existing fracture zones in the crust. This paper describes a new technique of frequency analysis of radiometric ages of crystalline rocks in the mountain ranges straddling the Indus-Tsangpo Suture Zone (ITSZ), the supposed line of collision between India and Asia, and shows that all the ranges from Karakoram to Lesser Himalaya across the ITSZ got uplifted simultaneously in a particular sequence. This contradicts the concept of suturing, places the ITSZ in the category of one of the intracrustal thrusts of the Himalayan orogenic system and establishes the family affinity between the Karakoram and the Himalaya. Analysis of stratigraphic and structural data points out that this family affinity is not confined to the ranges only but extends beyond into the foreland and oceanic basins as well. This paper also explains a number of apparent contradictions in terrain geomorphology, ophiolites in suture zones, thickness anomaly of Himalaya-derived sediments in eastern and western wings of terrestrial and oceanic basins to the south of the ranges, the status of Mid-oceanic Ridges in global tectonics, convergence aspect between Himalaya and India, nature of Foothills Fault and metamorphism of early Tertiary sediments in the Himalayan foreland basin.</subfield>
  </datafield>
  <datafield tag="540" ind1=" " ind2=" ">
   <subfield code="a">Geological Society of India, 2013</subfield>
  </datafield>
  <datafield tag="690" ind1=" " ind2="7">
   <subfield code="a">India-Asia collision</subfield>
   <subfield code="2">nationallicence</subfield>
  </datafield>
  <datafield tag="690" ind1=" " ind2="7">
   <subfield code="a">Endogenic process of orogeny</subfield>
   <subfield code="2">nationallicence</subfield>
  </datafield>
  <datafield tag="690" ind1=" " ind2="7">
   <subfield code="a">Himalaya-Karakoram affinity</subfield>
   <subfield code="2">nationallicence</subfield>
  </datafield>
  <datafield tag="690" ind1=" " ind2="7">
   <subfield code="a">Isotope geochronology</subfield>
   <subfield code="2">nationallicence</subfield>
  </datafield>
  <datafield tag="690" ind1=" " ind2="7">
   <subfield code="a">Ophiolites</subfield>
   <subfield code="2">nationallicence</subfield>
  </datafield>
  <datafield tag="690" ind1=" " ind2="7">
   <subfield code="a">Foothills fault</subfield>
   <subfield code="2">nationallicence</subfield>
  </datafield>
  <datafield tag="690" ind1=" " ind2="7">
   <subfield code="a">Metamorphism in foreland basin</subfield>
   <subfield code="2">nationallicence</subfield>
  </datafield>
  <datafield tag="690" ind1=" " ind2="7">
   <subfield code="a">Arabian Sea</subfield>
   <subfield code="2">nationallicence</subfield>
  </datafield>
  <datafield tag="690" ind1=" " ind2="7">
   <subfield code="a">Bay of Bengal</subfield>
   <subfield code="2">nationallicence</subfield>
  </datafield>
  <datafield tag="773" ind1="0" ind2=" ">
   <subfield code="t">Journal of the Geological Society of India</subfield>
   <subfield code="d">Springer-Verlag</subfield>
   <subfield code="g">81/3(2013-03-01), 337-349</subfield>
   <subfield code="x">0016-7622</subfield>
   <subfield code="q">81:3&lt;337</subfield>
   <subfield code="1">2013</subfield>
   <subfield code="2">81</subfield>
   <subfield code="o">12594</subfield>
  </datafield>
  <datafield tag="856" ind1="4" ind2="0">
   <subfield code="u">https://doi.org/10.1007/s12594-013-0044-4</subfield>
   <subfield code="q">text/html</subfield>
   <subfield code="z">Onlinezugriff via DOI</subfield>
  </datafield>
  <datafield tag="908" ind1=" " ind2=" ">
   <subfield code="D">1</subfield>
   <subfield code="a">research-article</subfield>
   <subfield code="2">jats</subfield>
  </datafield>
  <datafield tag="950" ind1=" " ind2=" ">
   <subfield code="B">NATIONALLICENCE</subfield>
   <subfield code="P">856</subfield>
   <subfield code="E">40</subfield>
   <subfield code="u">https://doi.org/10.1007/s12594-013-0044-4</subfield>
   <subfield code="q">text/html</subfield>
   <subfield code="z">Onlinezugriff via DOI</subfield>
  </datafield>
  <datafield tag="950" ind1=" " ind2=" ">
   <subfield code="B">NATIONALLICENCE</subfield>
   <subfield code="P">100</subfield>
   <subfield code="E">1-</subfield>
   <subfield code="a">Raiverman</subfield>
   <subfield code="D">V.</subfield>
   <subfield code="u">708 Maitri Apartment, 255 N.S.C. Bose Road, 700 047, Kolkata, India</subfield>
   <subfield code="4">aut</subfield>
  </datafield>
  <datafield tag="950" ind1=" " ind2=" ">
   <subfield code="B">NATIONALLICENCE</subfield>
   <subfield code="P">773</subfield>
   <subfield code="E">0-</subfield>
   <subfield code="t">Journal of the Geological Society of India</subfield>
   <subfield code="d">Springer-Verlag</subfield>
   <subfield code="g">81/3(2013-03-01), 337-349</subfield>
   <subfield code="x">0016-7622</subfield>
   <subfield code="q">81:3&lt;337</subfield>
   <subfield code="1">2013</subfield>
   <subfield code="2">81</subfield>
   <subfield code="o">12594</subfield>
  </datafield>
  <datafield tag="900" ind1=" " ind2="7">
   <subfield code="a">Metadata rights reserved</subfield>
   <subfield code="b">Springer special CC-BY-NC licence</subfield>
   <subfield code="2">nationallicence</subfield>
  </datafield>
  <datafield tag="898" ind1=" " ind2=" ">
   <subfield code="a">BK010053</subfield>
   <subfield code="b">XK010053</subfield>
   <subfield code="c">XK010000</subfield>
  </datafield>
  <datafield tag="949" ind1=" " ind2=" ">
   <subfield code="B">NATIONALLICENCE</subfield>
   <subfield code="F">NATIONALLICENCE</subfield>
   <subfield code="b">NL-springer</subfield>
  </datafield>
 </record>
</collection>
