Two diamictites, two cap carbonates, two δ13C excursions, two rifts: The Neoproterozoic Kingston Peak Formation, Death Valley, California

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Crustal Geodynamics Group, School of Geography and Geosciences, University of St. Andrews, St Andrews, Fife KY16 9ST, United Kingdom ^{[1
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Geology | / 4卷 / 339-342期

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[1] Two diamictites, two cap carbonates, two δ13C excursions, two rifts:: The Neoproterozoic Kingston Peak Formation, Death Valley, California
Prave, AR
GEOLOGY, 1999, 27 (04) : 339 - 342
[2] Two diamictites, two cap carbonates, two δ13C excursions, two rifts:: The Neoproterozoic Kingston Peak Formation, Death Valley, California:: Comment
Labotka, TC
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GEOLOGY, 2000, 28 (02) : 191 - 192
[3] Two diamictites, two cap carbonates, two δ13C excursions, two rifts:: The Neoproterozoic Kingston Peak Formation, Death Valley, California:: Reply
Prave, AR
GEOLOGY, 2000, 28 (02) : 192 - 192
[4] Geochronological constraints on Neoproterozoic rifting and onset of the Marinoan glaciation from the Kingston Peak Formation in Death Valley, California (USA)
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[5] Two-stage formation of Death Valley
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[6] δ13C and δD evidence for two series of PAH formation in the natural environments
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[7] Syn-rift mass flow generated 'tectonofacies' and 'tectonosequences' of the Kingston Peak Formation, Death Valley, California, and their bearing on supposed Neoproterozoic panglacial climates
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[8] Galactomannans from two species of Gleditsia studied by 13C NMR
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[9] After two decades a second anchor for the VPDB δ13C scale
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[10] Convenient preparation of amino acid derivatives with two 13C labels
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