ERRATUM: Jurassic–Cenozoic tectonics of the Pequop Mountains, NE Nevada, in the North American Cordillera hinterland

In Figures 13B and 13C on p. 2103, several unit contacts in the footwall of the Independence thrust were shown as thick and red (i.e., a fault), bounding the Ordovician strata (O), because of a conversion error. These lines should be thin and black, instead (i.e., a contact). The corrected figure follows.

• Publication year

  2022

• Venue

  Geosphere

• Publication date

  2022-02-18

• Fields of study

  Not labeled

• Identifiers
  DOI 10.1130/ges02307e.1
• External record

  Open on Semantic Scholar

• Source metadata

  Semantic Scholar

• No claims are published for this paper.

• No concepts are published for this paper.

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