Chapter 40 The Kingston Peak Formation in the eastern Death Valley region

2011 ◽  
Vol 36 (1) ◽  
pp. 449-458 ◽  
Author(s):  
David Mrofka ◽  
Martin Kennedy
Keyword(s):  
Death Valley ◽  
Kingston Peak Formation

Geochronological constraints on Neoproterozoic rifting and onset of the Marinoan glaciation from the Kingston Peak Formation in Death Valley, California (USA)

Geology ◽  
2020 ◽  
Vol 48 (11) ◽  
pp. 1083-1087 ◽  
Author(s):  
Lyle L. Nelson ◽  
Emily F. Smith ◽  
Eben B. Hodgin ◽  
James L. Crowley ◽  
Mark D. Schmitz ◽  
...  
Keyword(s):  
Thermal Ionization Mass Spectrometry ◽  
Death Valley ◽  
Snowball Earth ◽  
Ionization Mass ◽  
Glacial Deposit ◽  
Cap Carbonate ◽  
Depositional Age ◽  
Geochronological Constraints ◽  
Kingston Peak Formation ◽  
Discontinuous Fault

Abstract Death Valley (California, USA) hosts iconic Cryogenian snowball Earth deposits, but the lack of direct geochronological constraints has permitted a variety of correlations and age models. Here, we report two precise zircon U-Pb isotope dilution–thermal ionization mass spectrometry dates for the Kingston Peak Formation: a volcanic eruptive age of 705.44 ± 0.28 Ma from the synglacial Limekiln Spring Member, and a maximum depositional age of 651.69 ± 0.64 Ma from the nonglacial Thorndike submember, which is below the Wildrose diamictite. These dates confirm that the Limekiln Spring and Surprise Members were deposited during the Sturtian glaciation, while the Wildrose submember is a Marinoan glacial deposit, and the overlying Sentinel Peak Member of the Noonday Formation is a Marinoan cap carbonate. Additionally, the age from the Thorndike submember supersedes existing radioisotopic ages from the Datangpo Formation in South China as the youngest constraint on the onset of the Marinoan glaciation, demonstrating that the Cryogenian nonglacial interlude lasted for at least 9 m.y. and the Marinoan glaciation was <17 m.y. long. Cryogenian glaciation in western Laurentia occurred against the backdrop of ∼85 m.y. of episodic rift-related subsidence and magmatism within laterally discontinuous, fault-bound basins.

THE KINGSTON PEAK FORMATION AND CRYOGENIAN GLACIATION IN DEATH VALLEY

2018 ◽  
Author(s):  
Francis A. Macdonald ◽  
◽  
Lyle L. Nelson ◽  
Emily F. Smith
Keyword(s):  
Death Valley ◽  
Kingston Peak Formation

scholarly journals Supplemental Material: Geochronological constraints on Neoproterozoic rifting and onset of the Marinoan glaciation from the Kingston Peak Formation in Death Valley, California (USA)

2020 ◽  
Author(s):  
Lyle Nelson ◽  
et al.
Keyword(s):  
Analytical Methods ◽  
Death Valley ◽  
Data Tables ◽  
Geochronological Constraints ◽  
Kingston Peak Formation

Detailed analytical methods, compiled geochronology data and references, U-Pb geochronology data tables, and field and petrographic photographs.<br>

scholarly journals Supplemental Material: Geochronological constraints on Neoproterozoic rifting and onset of the Marinoan glaciation from the Kingston Peak Formation in Death Valley, California (USA)

2020 ◽  
Author(s):  
Lyle Nelson ◽  
et al.
Keyword(s):  
Analytical Methods ◽  
Death Valley ◽  
Data Tables ◽  
Geochronological Constraints ◽  
Kingston Peak Formation

Detailed analytical methods, compiled geochronology data and references, U-Pb geochronology data tables, and field and petrographic photographs.<br>

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

Geology ◽  
2000 ◽  
Vol 28 (2) ◽  
pp. 191-192
Author(s):  
Theodore C. Labotka ◽  
Deborah Bergfeld ◽  
Peter I. Nabelek ◽  
Deborah Bergfeld ◽  
Anthony R. Prave
Keyword(s):  
Death Valley ◽  
Cap Carbonates ◽  
Kingston Peak Formation
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