Matches in SemOpenAlex for { <https://semopenalex.org/work/W2107326815> ?p ?o ?g. }
- W2107326815 endingPage "664" @default.
- W2107326815 startingPage "652" @default.
- W2107326815 abstract "Research Article| May 01, 2014 Geochronologic and stratigraphic constraints on the Mesoproterozoic and Neoproterozoic Pahrump Group, Death Valley, California: A record of the assembly, stability, and breakup of Rodinia Robert C. Mahon; Robert C. Mahon 1Idaho State University Department of Geosciences, 921 S. 8th Ave., Stop 8072, Pocatello, Idaho 83209-8072, USA †Current address: University of Wyoming Department of Geology and Geophysics, Department 3006, 1000 University Ave., Laramie, Wyoming 82071, USA; e-mail: mahorobe@isu.edu; rmahon1@uwyo.edu. Search for other works by this author on: GSW Google Scholar Carol M. Dehler; Carol M. Dehler 2Utah State University Department of Geology, 4505 Old Main Hill, Logan, Utah 84322-4505, USA Search for other works by this author on: GSW Google Scholar Paul K. Link; Paul K. Link 1Idaho State University Department of Geosciences, 921 S. 8th Ave., Stop 8072, Pocatello, Idaho 83209-8072, USA Search for other works by this author on: GSW Google Scholar Karl E. Karlstrom; Karl E. Karlstrom 3University of New Mexico Department of Earth and Planetary Sciences, MSCO3-2040, Albuquerque, New Mexico 87131, USA Search for other works by this author on: GSW Google Scholar George E. Gehrels George E. Gehrels 4University of Arizona Department of Geosciences, 1040 E. 4th St., Tucson, Arizona 85721, USA Search for other works by this author on: GSW Google Scholar GSA Bulletin (2014) 126 (5-6): 652–664. https://doi.org/10.1130/B30956.1 Article history received: 07 Jul 2013 rev-recd: 03 Dec 2013 accepted: 08 Jan 2014 first online: 08 Mar 2017 Cite View This Citation Add to Citation Manager Share Icon Share Facebook Twitter LinkedIn MailTo Tools Icon Tools Get Permissions Search Site Citation Robert C. Mahon, Carol M. Dehler, Paul K. Link, Karl E. Karlstrom, George E. Gehrels; Geochronologic and stratigraphic constraints on the Mesoproterozoic and Neoproterozoic Pahrump Group, Death Valley, California: A record of the assembly, stability, and breakup of Rodinia. GSA Bulletin 2014;; 126 (5-6): 652–664. doi: https://doi.org/10.1130/B30956.1 Download citation file: Ris (Zotero) Refmanager EasyBib Bookends Mendeley Papers EndNote RefWorks BibTex toolbar search Search Dropdown Menu toolbar search search input Search input auto suggest filter your search All ContentBy SocietyGSA Bulletin Search Advanced Search Abstract The Pahrump Group in the Death Valley region of eastern California records a rich history of Mesoproterozoic to Neoproterozoic tectonic, climatic, and biotic events. These include the formation, stability, and onset of rifting of the Rodinia supercontinent, two potentially low-latitude glaciations correlative with global “snowball Earth” glacial intervals, and the onset of complex microbiota (e.g., testate amoebae). Poor direct age control, however, has significantly hindered the progress of understanding of these important stratigraphic units. New LA-ICPMS (laser ablation–inductively coupled plasma mass spectrometry) detrital zircon data from clastic units directly overlying a major unconformity within the Mesoproterozoic Crystal Spring Formation provide a maximum depositional age of 787 ± 11 Ma for the upper member of the Crystal Spring Formation. This unconformity, representing a duration of ≥300 Ma, is now recognized in sedimentary successions across southwestern Laurentia. These new age data, in addition to the distinct stratigraphic style above and below the unconformity, result in the proposed formal stratigraphic revision to elevate the upper member of the Crystal Spring Formation to the Neoproterozoic Horse Thief Springs Formation and separate it from the remainder of the underlying Mesoproterozoic Crystal Spring Formation (ca. 1100 Ma). New age relations and revised stratigraphic nomenclature significantly clarify stratigraphic and tectonic correlations and imply ca. 1250–1070 Ma assembly, 1070–780 Ma stability, and 780–600 Ma breakup of the supercontinent Rodinia along the southwestern Laurentian margin. You do not have access to this content, please speak to your institutional administrator if you feel you should have access." @default.
- W2107326815 created "2016-06-24" @default.
- W2107326815 creator A5006366882 @default.
- W2107326815 creator A5037780952 @default.
- W2107326815 creator A5041250552 @default.
- W2107326815 creator A5080699186 @default.
- W2107326815 creator A5090086069 @default.
- W2107326815 date "2014-02-27" @default.
- W2107326815 modified "2023-10-03" @default.
- W2107326815 title "Geochronologic and stratigraphic constraints on the Mesoproterozoic and Neoproterozoic Pahrump Group, Death Valley, California: A record of the assembly, stability, and breakup of Rodinia" @default.
- W2107326815 cites W1515908705 @default.
- W2107326815 cites W1596867262 @default.
- W2107326815 cites W1966339226 @default.
- W2107326815 cites W1966526622 @default.
- W2107326815 cites W1981468283 @default.
- W2107326815 cites W1988308108 @default.
- W2107326815 cites W2003863444 @default.
- W2107326815 cites W2005535021 @default.
- W2107326815 cites W2008510365 @default.
- W2107326815 cites W2018623014 @default.
- W2107326815 cites W2031153814 @default.
- W2107326815 cites W2037065936 @default.
- W2107326815 cites W2039132540 @default.
- W2107326815 cites W2040589286 @default.
- W2107326815 cites W2048240400 @default.
- W2107326815 cites W2049439225 @default.
- W2107326815 cites W2051164176 @default.
- W2107326815 cites W2053844254 @default.
- W2107326815 cites W2067675545 @default.
- W2107326815 cites W2075694434 @default.
- W2107326815 cites W2088111195 @default.
- W2107326815 cites W2092672858 @default.
- W2107326815 cites W2094932813 @default.
- W2107326815 cites W2096389073 @default.
- W2107326815 cites W2098796617 @default.
- W2107326815 cites W2104917892 @default.
- W2107326815 cites W2110586434 @default.
- W2107326815 cites W2117123644 @default.
- W2107326815 cites W2117941890 @default.
- W2107326815 cites W2123794017 @default.
- W2107326815 cites W2126663701 @default.
- W2107326815 cites W2138210062 @default.
- W2107326815 cites W2141527546 @default.
- W2107326815 cites W2142409030 @default.
- W2107326815 cites W2159870720 @default.
- W2107326815 cites W2162531714 @default.
- W2107326815 cites W2162869345 @default.
- W2107326815 cites W2164913450 @default.
- W2107326815 cites W2167810665 @default.
- W2107326815 cites W2168346738 @default.
- W2107326815 cites W2180371742 @default.
- W2107326815 cites W2213808876 @default.
- W2107326815 cites W2313716199 @default.
- W2107326815 cites W2441057870 @default.
- W2107326815 cites W2480704990 @default.
- W2107326815 cites W2498909273 @default.
- W2107326815 cites W3120393643 @default.
- W2107326815 cites W4231820044 @default.
- W2107326815 cites W78869628 @default.
- W2107326815 doi "https://doi.org/10.1130/b30956.1" @default.
- W2107326815 hasPublicationYear "2014" @default.
- W2107326815 type Work @default.
- W2107326815 sameAs 2107326815 @default.
- W2107326815 citedByCount "44" @default.
- W2107326815 countsByYear W21073268152014 @default.
- W2107326815 countsByYear W21073268152015 @default.
- W2107326815 countsByYear W21073268152016 @default.
- W2107326815 countsByYear W21073268152017 @default.
- W2107326815 countsByYear W21073268152018 @default.
- W2107326815 countsByYear W21073268152019 @default.
- W2107326815 countsByYear W21073268152020 @default.
- W2107326815 countsByYear W21073268152021 @default.
- W2107326815 countsByYear W21073268152022 @default.
- W2107326815 countsByYear W21073268152023 @default.
- W2107326815 crossrefType "journal-article" @default.
- W2107326815 hasAuthorship W2107326815A5006366882 @default.
- W2107326815 hasAuthorship W2107326815A5037780952 @default.
- W2107326815 hasAuthorship W2107326815A5041250552 @default.
- W2107326815 hasAuthorship W2107326815A5080699186 @default.
- W2107326815 hasAuthorship W2107326815A5090086069 @default.
- W2107326815 hasConcept C109007969 @default.
- W2107326815 hasConcept C11413529 @default.
- W2107326815 hasConcept C127313418 @default.
- W2107326815 hasConcept C151730666 @default.
- W2107326815 hasConcept C161191863 @default.
- W2107326815 hasConcept C166957645 @default.
- W2107326815 hasConcept C2779241739 @default.
- W2107326815 hasConcept C41008148 @default.
- W2107326815 hasConcept C48103436 @default.
- W2107326815 hasConcept C50682988 @default.
- W2107326815 hasConcept C52119013 @default.
- W2107326815 hasConcept C67101536 @default.
- W2107326815 hasConcept C95457728 @default.
- W2107326815 hasConceptScore W2107326815C109007969 @default.
- W2107326815 hasConceptScore W2107326815C11413529 @default.
- W2107326815 hasConceptScore W2107326815C127313418 @default.
- W2107326815 hasConceptScore W2107326815C151730666 @default.
- W2107326815 hasConceptScore W2107326815C161191863 @default.