Geochronologic Age Constraints on Tectonostratigraphic Units of the Central Virginia Piedmont, USA

Professional Paper 1861
By: , and 

Links

  • Document: Report (9.51 MB pdf)
  • Tables:
    • Table 2 (98.5 KB xlsx) - Isotopic data for all analyses by laser ablation-inductively coupled plasma-mass spectrometry at the U.S. Geological Survey Central Mineral and Environmental Resources Science Center Isotope Laboratory in Denver, Colorado
    • Table 3 (447 KB xlsx) - Isotopic data for all analyses by secondary ionization mass spectrometry on the U.S. Geological Survey/Stanford sensitive high-resolution ion microprobe-reverse geometry
  • Open Access Version: Publisher Index Page
  • Download citation as: RIS | Dublin Core

Abstract

New geologic mapping coupled with uranium-lead (U-Pb) zircon geochronology (sensitive high-resolution ion microprobe-reverse geometry [SHRIMP-RG] and laser ablation-inductively coupled plasma-mass spectrometry [LA-ICP-MS]) analyses of 10 samples, provides new constraints on the tectonostratigraphic framework of the central Virginia Piedmont. Detrital zircon analysis confirms that the Silurian-Devonian Quantico Formation is a postorogenic successor basin, with zircons derived primarily from Ordovician Chopawamsic Formation volcanic rocks. Detrital zircons from strata of the Long Island syncline, previously mapped as a separate successor basin, have a peri-Gondwanan component distinct from Laurentian-sourced rocks of the Potomac terrane to the west. Volcanism of the Chopawamsic Formation spanned at least 14 million years during the Ordovician. The Chopawamsic Formation contains sheet-like Late Ordovician-Silurian granodioritic and tonalitic intrusions that were once mapped as Carboniferous. Biotite-muscovite migmatitic paragneiss, which borders the Chopawamsic Formation on its southeast side and also occurs east of the Lakeside fault, preserves evidence of Silurian deformation and metamorphism, with a Carboniferous (Alleghanian) overprint. Limited SHRIMP-RG analysis of detrital zircons from this paragneiss yields a Laurentian (Mesoproterozoic) signature, which suggests that the structurally concordant contact between volcanic rocks of the Chopawamsic Formation and paragneiss is either a pre-Alleghanian fault or an unconformity.

Suggested Citation

Carter, M.W., McAleer, R.J., Holm-Denoma, C.S., Spears, D.B., Regan, S.P., Burton, W.C., and Evans, N.H., 2020, Geochronologic age constraints on tectonostratigraphic units of the central Virginia Piedmont, USA: U.S. Geological Survey Professional Paper 1861, 28 p., https://doi.org/10.3133/pp1861.

ISSN: 2330-7102 (online)

Study Area

Table of Contents

  • Acknowledgments
  • Abstract
  • Introduction
  • Analytical Methods
  • Results
  • Discussion
  • Conclusions
  • References Cited
  • Appendix 1. Laser Ablation-Inductively Coupled Plasma-Mass Spectrometry (LA-ICP-MS) Methodology
  • Appendix 2. Secondary Ionization Mass Spectrometry Methodology

Additional publication details

Publication type Report
Publication Subtype USGS Numbered Series
Title Geochronologic age constraints on tectonostratigraphic units of the central Virginia Piedmont, USA
Series title Professional Paper
Series number 1861
DOI 10.3133/pp1861
Year Published 2020
Language English
Publisher U.S. Geological Survey
Publisher location Reston, VA
Contributing office(s) Eastern Geology and Paleoclimate Science Center
Description Report: vi, 28 p.; 2 Tables
Country United States
State Virginia
Online Only (Y/N) Y
Additional Online Files (Y/N) Y
Google Analytic Metrics Metrics page