Provenance of the Granjeno Schist, Ciudad Victoria, México: Detrital zircon U-Pb age constraints and implications for the Paleozoic paleogeography of the Rheic Ocean

Special Paper of the Geological Society of America

Volumn 423, Issue , 2007, Pages 453-464

  Nance, R Damian ^a   Fernández Suárez, Javier ^b   Keppie, J Duncan ^c   Storey, Craig ^d,f   Jeffries, Teresa E ^e  

^a OHIO UNIVERSITY   (United States)

^b UNIVERSIDAD COMPLUTENSE DE MADRID   (Spain)

^c UNIVERSIDAD NACIONAL AUTÓNOMA DE MÉXICO   (Mexico)

^d OPEN UNIVERSITY   (United Kingdom)

^e DEPARTMENT OF LIFE SCIENCES   (United Kingdom)

^f UNIVERSITY OF BRISTOL   (United Kingdom)

Author keywords

Detrital zircons; Granjeno Schist; M xico; Paleozoic; Rheic Ocean

Indexed keywords

BINARY ALLOYS; INDUCTIVELY COUPLED PLASMA; LASER ABLATION; LEAD ALLOYS; MAGNESITE; MASS SPECTROMETERS; MASS SPECTROMETRY; SILICATE MINERALS; URANIUM ALLOYS; ZIRCON;

DETRITAL ZIRCON; FOLD-THRUST BELTS; GRANJENO SCHIST; INDUCTIVELY COUPLED PLASMA MASS SPECTROSCOPIES; NEOPROTEROZOIC; PALEOZOIC; RHEIC OCEAN; YUCATAN PENINSULA;

OCEANOGRAPHY;

AGE; ANTICLINE; CAMBRIAN; GNEISS; PALEOGEOGRAPHY; PALEOZOIC; PHYLLITE; PROVENANCE; SCHIST; SILURIAN; TERRANE; ZIRCON;

CIUDAD VICTORIA; MEXICO [NORTH AMERICA]; SIERRA MADRE [MEXICO]; SOUTH AMERICA; TAMAULIPAS; YUCATAN PENINSULA;

CELTIS PALLIDA;

EID: 39149097628     PISSN: 00721077     EISSN: None     Source Type: Book Series    
DOI: 10.1130/2007.2423(22)     Document Type: Conference Paper

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