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Publications tagged with [geochronology]

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QUATERNARY FAULTING IN QUEEN VALLEY, CALIFORNIA-NEVADA: IMPLICATIONS FOR KINEMATICS OF FAULT-SLIP TRANSFER IN THE EASTERN CALIFORNIA SHEAR ZONE-WALKER LANE BELT (2009)
In this paper new geologic map, tectonic, geomorphologic, and terrestrial cosmogenic nuclide(TCN) geochronologic data document the geometry, style, kinematics, and slip rates on late Quaternary faults within the Queen Valley, California-Nevada area.
Reference: GSA Bulletin; March/April 2009; v. 121; no. 3/4; p. 599-614
A NEW CHRONOLOGY FOR THE AGE OF APPALACHIAN EROSIONAL SURFACES DETERMINED BY COSMOGENIC NUCLIDES IN CAVE SEDIMENTS (2007)
Relative chronology of landscape evolution across the unglaciated Appalachian plateaus of Kentucky and Tennessee.
Filed under: Geology -  General Geology
Reference: "Earth Surface Processes and Landforms Earth Surf. Process. Landforms 32, 874-887 (2007)"
LATE QUATERNARY SLIP RATES ALONG THE SIERRA NEVADA FRONTAL FAULTZONE, CALIFORNIA: SLIP PARTITIONING ACROSS THE WESTERN MARGIN OF THEEASTERN CALIFORNIA SHEAR ZONE - BASIN AND RANGE PROVINCE (2007)
Le K. , Lee J. et al.  
This paper is about new geologic mapping, tectonic geomorphologic, and cosmogenic radionuclide geochronologic data that provide the first numerical constraints on late Quaternary vertical slip and horizontal extension rates across the southern Sierra Nevada ...
Reference: GSA Bulletin; January/February 2007; v. 119; no. 1/2; p. 240-256.
GEOCHEMISTRY AND GEOCHRONOLOGY OF THE RATHJEN GNEISS: IMPLICATIONS FOR THE EARLY TECTONIC EVOLUTION OF THE DELAMERIAN OROGEN (1999)
This paper is about the Rathjen Gneiss which the oldest and structurally most complex of the granitic intrusives in the southern Adelaide Fold - Thrust Belt and therefore provides an important constraint on the timing of the Delamerian Orogen.
Reference: Australian Journal of Earth Sciences (1999) 46, 377-389
PETROLOGY AND GEOCHEMISTRY OF THE TROMY GNEISS COMPLEX, SOUTH NORWAY, AN ALLEGED EXAMPLE OF PROTEROZOIC DEPLETED LOWER CONTINENTAL CRUST (1999)
A granulite-facies Precambrian meta-igneous gneiss complex at Tromy, South Norway, which was previously assumed to represent a fragment of strongly large ion lithophile element (LILE)-depleted lower continental crust, has been reinvestigated using major and ...
Reference: JOURNAL OF PETROLOGY VOLUME 40 NUMBER 6 PAGES 909-933, 1999