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 <front>
  <journal-meta>
   <journal-id journal-id-type="publisher-id">Russian Journal of Earth Sciences</journal-id>
   <journal-title-group>
    <journal-title xml:lang="en">Russian Journal of Earth Sciences</journal-title>
    <trans-title-group xml:lang="ru">
     <trans-title>Russian Journal of Earth Sciences</trans-title>
    </trans-title-group>
   </journal-title-group>
   <issn publication-format="online">1681-1208</issn>
  </journal-meta>
  <article-meta>
   <article-id pub-id-type="publisher-id">46519</article-id>
   <article-id pub-id-type="doi">10.2205/2020ES000666</article-id>
   <article-categories>
    <subj-group subj-group-type="toc-heading" xml:lang="ru">
     <subject>ОРИГИНАЛЬНЫЕ СТАТЬИ</subject>
    </subj-group>
    <subj-group subj-group-type="toc-heading" xml:lang="en">
     <subject>ORIGINAL ARTICLES</subject>
    </subj-group>
    <subj-group>
     <subject>ОРИГИНАЛЬНЫЕ СТАТЬИ</subject>
    </subj-group>
   </article-categories>
   <title-group>
    <article-title xml:lang="en">Geochemistry and petrology of two kimberlites at Krishtipadu from Gooty cluster, Andhra Pradesh, southern India - evidence of kimberlite magmatism and a possible carbonatite association within Palaeoproterozoic lower Cuddapah basin</article-title>
    <trans-title-group xml:lang="ru">
     <trans-title>Geochemistry and petrology of two kimberlites at Krishtipadu from Gooty cluster, Andhra Pradesh, southern India - evidence of kimberlite magmatism and a possible carbonatite association within Palaeoproterozoic lower Cuddapah basin</trans-title>
    </trans-title-group>
   </title-group>
   <contrib-group content-type="authors">
    <contrib contrib-type="author">
     <name-alternatives>
      <name xml:lang="ru">
       <surname>Phani</surname>
       <given-names>P Ramesh Chandra</given-names>
      </name>
      <name xml:lang="en">
       <surname>Phani</surname>
       <given-names>P Ramesh Chandra</given-names>
      </name>
     </name-alternatives>
     <email>phaniprc@gmail.com</email>
     <xref ref-type="aff" rid="aff-1"/>
    </contrib>
    <contrib contrib-type="author">
     <name-alternatives>
      <name xml:lang="ru">
       <surname>Sengupta</surname>
       <given-names>Prabir </given-names>
      </name>
      <name xml:lang="en">
       <surname>Sengupta</surname>
       <given-names>Prabir </given-names>
      </name>
     </name-alternatives>
     <xref ref-type="aff" rid="aff-2"/>
    </contrib>
    <contrib contrib-type="author">
     <name-alternatives>
      <name xml:lang="ru">
       <surname>Basu</surname>
       <given-names>Sudeshna </given-names>
      </name>
      <name xml:lang="en">
       <surname>Basu</surname>
       <given-names>Sudeshna </given-names>
      </name>
     </name-alternatives>
     <xref ref-type="aff" rid="aff-3"/>
    </contrib>
   </contrib-group>
   <aff-alternatives id="aff-1">
    <aff>
     <institution xml:lang="ru">Cyient Limited</institution>
     <country>ru</country>
    </aff>
    <aff>
     <institution xml:lang="en">Cyient Limited</institution>
     <country>ru</country>
    </aff>
   </aff-alternatives>
   <aff-alternatives id="aff-2">
    <aff>
     <institution xml:lang="ru">Bedrock Mineral Resource Consulting</institution>
     <country>ru</country>
    </aff>
    <aff>
     <institution xml:lang="en">Bedrock Mineral Resource Consulting</institution>
     <country>ru</country>
    </aff>
   </aff-alternatives>
   <aff-alternatives id="aff-3">
    <aff>
     <institution xml:lang="ru">Cairn India Oil &amp; Gas, Vedanta Limited</institution>
     <country>ru</country>
    </aff>
    <aff>
     <institution xml:lang="en">Cairn India Oil &amp; Gas, Vedanta Limited</institution>
     <country>ru</country>
    </aff>
   </aff-alternatives>
   <volume>20</volume>
   <issue>3</issue>
   <fpage>1</fpage>
   <lpage>14</lpage>
   <history>
    <date date-type="received" iso-8601-date="2021-10-29T12:47:41+03:00">
     <day>29</day>
     <month>10</month>
     <year>2021</year>
    </date>
   </history>
   <self-uri xlink:href="https://rjes.ru/en/nauka/article/46519/view">https://rjes.ru/en/nauka/article/46519/view</self-uri>
   <abstract xml:lang="ru">
    <p>This paper addresses geochemical and petrological aspects of two outcropping kimberlites (5023 and 5119) of the Gooty cluster, emplaced in carbonate sediments of Vempalli Formation of lower Cuddapah basin at Krishtipadu, Anantapur district, Andhra Pradesh, southern India. These pipes were discovered by the Rio Tinto Exploration Group in the recent past. The 5023 kimberlite is enriched in olivine and serpentine while the 5119 pipe possesses haematitised olivine pseudomorphs. The field, textural characteristics and whole rock geochemistry qualify both the pipes for hypabyssal kimberlite breccias of Group-I type similar to world's classical occurrences. The carbon and oxygen stable isotope data, aided with field and petrological studies, indicates existence of possible carbonatite (sovite) phase associated with the 5119 kimberlite. The two kimberlites appear to be originated from a low degree of partial melting ranging from 0.5 to 2.5%. Enrichment of LREE with a high LREE/HREE ratio indicates fractionation at the mantle source region. Whole rock geochemistry supports their diamondiferous nature. Presence of crustal xenoliths post-dates subsequent emplacement of the two pipes to lower Cuddapah sedimentation (2.4 Ga), manifesting kimberlite magmatism. These pipes are the only known Group-I kimberlites from the Proterozoic Cuddapah Basin and therefore warrant detailed investigations.</p>
   </abstract>
   <trans-abstract xml:lang="en">
    <p>This paper addresses geochemical and petrological aspects of two outcropping kimberlites (5023 and 5119) of the Gooty cluster, emplaced in carbonate sediments of Vempalli Formation of lower Cuddapah basin at Krishtipadu, Anantapur district, Andhra Pradesh, southern India. These pipes were discovered by the Rio Tinto Exploration Group in the recent past. The 5023 kimberlite is enriched in olivine and serpentine while the 5119 pipe possesses haematitised olivine pseudomorphs. The field, textural characteristics and whole rock geochemistry qualify both the pipes for hypabyssal kimberlite breccias of Group-I type similar to world's classical occurrences. The carbon and oxygen stable isotope data, aided with field and petrological studies, indicates existence of possible carbonatite (sovite) phase associated with the 5119 kimberlite. The two kimberlites appear to be originated from a low degree of partial melting ranging from 0.5 to 2.5%. Enrichment of LREE with a high LREE/HREE ratio indicates fractionation at the mantle source region. Whole rock geochemistry supports their diamondiferous nature. Presence of crustal xenoliths post-dates subsequent emplacement of the two pipes to lower Cuddapah sedimentation (2.4 Ga), manifesting kimberlite magmatism. These pipes are the only known Group-I kimberlites from the Proterozoic Cuddapah Basin and therefore warrant detailed investigations.</p>
   </trans-abstract>
   <kwd-group xml:lang="ru">
    <kwd>Kimberlite</kwd>
    <kwd>carbonatite</kwd>
    <kwd>archetypal Group-I</kwd>
    <kwd>Gooty Kimberlite Cluster</kwd>
    <kwd>lowerCuddapah basin</kwd>
    <kwd>stable isotope</kwd>
    <kwd>Palaeoproterozoic</kwd>
   </kwd-group>
   <kwd-group xml:lang="en">
    <kwd>Kimberlite</kwd>
    <kwd>carbonatite</kwd>
    <kwd>archetypal Group-I</kwd>
    <kwd>Gooty Kimberlite Cluster</kwd>
    <kwd>lowerCuddapah basin</kwd>
    <kwd>stable isotope</kwd>
    <kwd>Palaeoproterozoic</kwd>
   </kwd-group>
   <funding-group>
    <funding-statement xml:lang="en">The successful discovery of Gooty kimberlite cluster is accredited to Rio Tinto Exploration (India). The primary intension of this article is to provide first hand data of the two pipes of the Gooty cluster. As these deposits are currently in free-hold area, the authors take liberty to publish this paper and whole heartedly thank Rio Tinto Exploration India Pvt. Ltd., Bangalore for giving them an opportunity to work as geologists, in diamond exploration projects, during the years 2001-2009. Thanks to Dr. Gargi Mishra, University of Johannesburg, S.A. for initial review on the manuscript. IRMS Lab, Wadia Institute of Himalayan Geology, Dehradun is thanked for stable isotope analyses. PRCP thanks Cyient Limited for facilitating IT resources and Prof. Mdabhooshi Srinivas, former Head, Dept. of Geology, Osmania University, Hyderabad for petrological microscope facility.</funding-statement>
   </funding-group>
  </article-meta>
 </front>
 <body>
  <p></p>
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