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  <namePart>Darijanto, Totok</namePart>
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   <placeTerm type="text">Bandung</placeTerm>
   <publisher>ITB - Departemen Teknik Pertambangan</publisher>
   <dateIssued>[1998]</dateIssued>
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  <extent>28 hlm. : ilus. ; 29 cm</extent>
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 <note>The structure of parent rock as well as the morphological situatio influence considerably for the development of lateric horizon. A characteristic profile of laterite deposit Gebe consist of (1-18m) saprolite zone at the bottom and (1-13m) limonite zone at the top of the profile.&#13;
&#13;
Geostatistical investigations to the lateral distribution of nickel and cobalt content as well as thickness of limonite and saprolite zone give quantitatively information, such as shown by their experimental variograms.</note>
 <note type="statement of responsibility">Institut Teknologi Bandung</note>
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  <geographic>Pulau Gebe</geographic>
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  <topic>Peninjauan Geologi</topic>
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  <topic>SKIP/Peninjauan/DD</topic>
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  <topic>Halmahera Tengah</topic>
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