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  <controlfield tag="008">260224s2011    xxu                      </controlfield>
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    <subfield code="a">Three-dimensional seismic geomorphology and analysis of the Ordovician paleokarst drainage system in the central Tabei Uplift, northern Tarim Basin, western China</subfield>
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    <subfield code="c">dic. 2011</subfield>
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  <datafield tag="270" ind1=" " ind2=" ">
    <subfield code="a">27/03/2012 ; 27/03/2012</subfield>
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    <subfield code="a">22 p. ; 2061-2083</subfield>
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    <subfield code="a">Transcripci&#xF3;n del resumen del autor: High-quality three-dimensional seismic data acquired in the central Tabei Uplift, Tarim Basin, western China, provide a rare opportunity to characterize in exceptional detail the three-dimensional geomorphology of a deeply buried (5500&amp;#x96;6500 m [18,045&amp;#x96;21,325 ft]) Ordovician unconformity and the related paleokarst drainage system. An integrated approach was applied that emphasized integration of seismic data with available conventional core, wireline logs, and age-equivalent outcrops. The exceptional quality of the seismic data allowed a seismic detection limit of karstified features of less than 75 &amp;#xD7; 75 m (246 &amp;#xD7; 246 ft) horizontally and 6 m (20 ft) vertically. Interpreted geomorphologic and depositional elements include fluvial channels and canyons, fluvial valleys, sinkholes, and tower karsts and hills. The modern tower karst-drainage system in Guilin, China, is very similar to the mapped Ordovician karst-drainage system and is used as a modern analog. The interaction between the surface karst-drainage system and the shallow-subsurface cave-passage system is evidenced by the observation that surface canyons appear to initiate in areas associated with intense sinkhole development. Also, surface river valleys tend to correspond to dip-oriented surface depressions partly related to near-surface cave collapse. During burial into the deeper subsurface, the combination of intrastratal collapse (karstified strata) and suprastratal collapse (postkarst-deposited strata) created large damage zones hundreds of meters thick and kilometers wide. Coalesced-collapsed paleocave systems can be interpreted from the unique circular pattern of faults (observed in map view) that are associated with seismic bright spots.</subfield>
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    <subfield code="g">95</subfield>
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    <subfield code="c">ARTICULO</subfield>
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    <subfield code="a">Zeng, Hongliu</subfield>
    <subfield code="9">26057</subfield>
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    <subfield code="a">Loucks, Robert</subfield>
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    <subfield code="a">Janson, Xavier</subfield>
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    <subfield code="a">Wang, Guizhong</subfield>
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    <subfield code="a">Xia, Yiping</subfield>
    <subfield code="9">52229</subfield>
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    <subfield code="a">Yuan, Bingheng</subfield>
    <subfield code="9">52230</subfield>
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    <subfield code="a">Xu, Ligui</subfield>
    <subfield code="9">52231</subfield>
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    <subfield code="c">186902</subfield>
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    <subfield code="7">0</subfield>
    <subfield code="9">254721</subfield>
    <subfield code="a">BAAB</subfield>
    <subfield code="b">BAAB</subfield>
    <subfield code="d">2026-03-06</subfield>
    <subfield code="j">200059007</subfield>
    <subfield code="l">0</subfield>
    <subfield code="p">200059007</subfield>
    <subfield code="r">2026-03-06 00:15:03</subfield>
    <subfield code="w">2026-03-06</subfield>
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