The Terrane Puzzle: New Perspectives on Paleontology and Stratigraphy from the North American Cordillera

Significance of detrital zircons in Upper Devonian ocean-basin strata of the Sonora allochthon and Lower Permian synorogenic strata of the Mina México foredeep, central Sonora, México
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Published:July 01, 2008
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CiteCitation
Forrest G. Poole, George E. Gehrels, John H. Stewart, 2008. "Significance of detrital zircons in Upper Devonian ocean-basin strata of the Sonora allochthon and Lower Permian synorogenic strata of the Mina México foredeep, central Sonora, México", The Terrane Puzzle: New Perspectives on Paleontology and Stratigraphy from the North American Cordillera, Robert B. Blodgett, George D. Stanley, Jr.
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U-Pb isotopic dating of detrital zircons from a conglomeratic barite sandstone in the Sonora allochthon and a calciclastic sandstone in the Mina México foredeep of the Minas de Barita area reveals two main age groups in the Upper Devonian part of the Los Pozos Formation, 1.73–1.65 Ga and 1.44–1.42 Ga; and three main age groups in the Lower Permian part of the Mina México Formation, 1.93–1.91 Ga, 1.45–1.42 Ga, and 1.1–1.0 Ga. Small numbers of zircons with ages of 2.72–2.65 Ga, 1.30–1.24 Ga, ca. 2.46 Ga, ca. 1.83 Ga, and ca. 0.53 Ga are also present in the Los Pozos...
- absolute age
- accretionary wedges
- allochthons
- basins
- clastic rocks
- conglomerate
- dates
- depositional environment
- detritus
- Devonian
- fore-arc basins
- Grenvillian Orogeny
- Laurentia
- Lower Permian
- marine environment
- Mexico
- nesosilicates
- orogeny
- orthosilicates
- paleogeography
- Paleozoic
- Permian
- Precambrian
- Proterozoic
- provenance
- sandstone
- sedimentary rocks
- shelf environment
- silicates
- Sonora Mexico
- syntectonic processes
- U/Pb
- Upper Devonian
- upper Precambrian
- zircon
- zircon group
- Mina Mexico Formation
- Los Pozos Formation