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<md:lastName>Riech</md:lastName>
<md:firstName>Volkher</md:firstName>
</md:author>
<md:year>1981</md:year>
<md:title>(Table 1) Characteristics of silicified sediments at DSDP Site 61-462 according to host-rock lithology, opal-CT-to-quartz ratio, and the origin of the quartz phase</md:title>
<md:type id="dataset.reftype10" includeInCitation="true">dataset</md:type>
<md:URI>https://doi.org/10.1594/PANGAEA.819840</md:URI>
<md:supplementTo id="ref60558">
<md:author id="ref60558.author21499">
<md:lastName>Riech</md:lastName>
<md:firstName>Volkher</md:firstName>
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<md:year>1981</md:year>
<md:title>Siliceous sediments from the Nauru Basin: Diagenetic alteration of biogenic opal and authigenesis of silica and silicates</md:title>
<md:type id="ref60558.reftype15">book chapter</md:type>
<md:source>In: Larson, RL; Schlanger, SO; et al. (eds.), Initial Reports of the Deep Sea Drilling Project (U.S. Govt. Printing Office)</md:source>
<md:volume>61</md:volume>
<md:URI>https://doi.org/10.2973/dsdp.proc.61.109.1981</md:URI>
<md:pages>523-531</md:pages>
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<md:abstract>This study deals with the mineralogical variability of siliceous and zeolitic sediments, porcellanites, and cherts at small intervals in the continuously cored sequence of Deep Sea Drilling Project Site 462. Skeletal opal is preserved down to a maximum burial depth of 390 meters (middle Eocene). Below this level, the tests are totally dissolved or replaced and filled by opal-CT, quartz, clinoptilolite, and calcite. Etching of opaline tests does not increase continously with deeper burial. Opal solution accompanied by a conspicuous formation of authigenic clinoptilolite has a local maximum in Core 16 (150 m). A causal relationship with the lower Miocene hiatus at this level is highly probable. 
Oligocene to Cenomanian sediments represent an intermediate stage of silica diagenesis: the opal-CT/quartz ratios of the silicified rocks are frequently greater than 1, and quartz filling pores or replacing foraminifer tests is more widespread than quartz which converted from an opal-CT precursor. 
As at other sites, there is a marked discontinuity of the transitions from biogenic opal via opal-CT to quartz with increasing depth of burial. Layers with unaltered opal-A alternate with porcellanite beds; the intensity of the opal-CT-to-quartz transformation changes very rapidly from horizon to horizon and obviously is not correlated with lithologic parameters. 
The silica for authigenic clinoptilolite was derived from biogenic opal and decaying volcanic components.</md:abstract>
<md:extent>
<md:geographic>
<md:westBoundLongitude>165.0305</md:westBoundLongitude>
<md:eastBoundLongitude>165.0317</md:eastBoundLongitude>
<md:southBoundLatitude>7.2375</md:southBoundLatitude>
<md:northBoundLatitude>7.2417</md:northBoundLatitude>
<md:meanLongitude>165.03109999999998</md:meanLongitude>
<md:meanLatitude>7.239599999999999</md:meanLatitude>
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<md:temporal>
<md:minDateTime>1978-05-28T00:00:00</md:minDateTime>
<md:maxDateTime>1978-06-09T00:00:00</md:maxDateTime>
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<md:min>-5181.0</md:min>
<md:max>-5177.0</md:max>
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<md:topoType id="topotype1">not specified</md:topoType>
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<md:label>DSDP</md:label>
<md:name>Deep Sea Drilling Project</md:name>
<md:URI>https://www.deepseadrilling.org/</md:URI>
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<md:name>Deep Sea Drilling Project</md:name>
<md:optionalName>DSDP</md:optionalName>
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<md:event displayTypeName="Event" id="event74899" typeName="Generic Event">
<md:label>61-462</md:label>
<md:latitude>7.2375</md:latitude>
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<md:dateTime>1978-05-28T00:00:00</md:dateTime>
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<md:dateTime>1978-05-22T00:00:00</md:dateTime>
<md:start warning="deprecated">1978-05-22</md:start>
<md:dateTime2>1978-07-29T00:00:00</md:dateTime2>
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<md:responsible>Larson, Roger L</md:responsible>
<md:chiefScientist warning="deprecated">Larson, Roger L</md:chiefScientist>
<md:responsible>Schlanger, Seymour O</md:responsible>
<md:chiefScientist warning="deprecated">Schlanger, Seymour O</md:chiefScientist>
<md:attribute attid="76863" name="Report">doi:10.2973/dsdp.proc.61.1981</md:attribute>
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<md:name>Glomar Challenger</md:name>
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<md:name>Drilling/drill rig</md:name>
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<md:attribute attid="19162" name="Penetration">617 m</md:attribute>
<md:attribute attid="19163" name="Recovery">386 m</md:attribute>
<md:comment>70 cores; 627.4 m cored; 0 m drilled; 61.5 % recovery</md:comment>
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<md:attribute attid="19162" name="Penetration">1068.5 m</md:attribute>
<md:attribute attid="19163" name="Recovery">344 m</md:attribute>
<md:comment>90 cores; 619.5 m cored; 14.5 m drilled; 55.5 % recovery</md:comment>
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<md:name>Creative Commons Attribution 3.0 Unported</md:name>
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<md:comment>- = no data, + = least abundant, ++++ = most abundant, ? = unknowns.</md:comment>
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<md:lastName>Riech</md:lastName>
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<md:comment>Of silicified rock</md:comment>
<md:caption>Lithology (Of silicified rock, X-ray dif...)</md:caption>
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<md:comment>Calcareous</md:comment>
<md:caption>Main lith (Calcareous, X-ray diffraction...)</md:caption>
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<md:comment>Siliceous</md:comment>
<md:caption>Main lith (Siliceous, X-ray diffraction ...)</md:caption>
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<md:comment>Early Diagenetic</md:comment>
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<md:name>Molar Concentration</md:name>
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<md:comment>Opal-CT/quartz ratio</md:comment>
<md:caption>- (Opal-CT/quartz ratio, X-ray d...)</md:caption>
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<md:comment>Stage of opal-CT - quartz transformation: + = small amount of opal-CT starts to transform into quartz, ++++ = all opal-CT transformed into quartz</md:comment>
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