CLOSURE, AGE2EDOT, and RESPTIME

June 24, 2007

Download Closure Programs here (1.4 Mb)

INTRODUCTION
CLOSURE, AGE2EDOT, and RESPTIME are a set of simple programs that were first
developed in Brandon et al. (1998). They were designed to help demonstrate the
influence of steady and transient erosion on fission-track (FT) cooling ages.
The programs have since been extended to include (U-Th)/He and 40Ar/39Ar ages,
as well as FT ages. The programs now include modern diffusion data for all of
the minerals commonly dated for thermochronometry, ranging from He dating of
apatite to Ar dating of hornblende.

CLOSURE is a standard Windows-style program, whereas AGE2EDOT and RESPTIME
are console-style programs. All of the programs are compiled for the Windows
operating system. Each consists of a single exe file. Setup involves copying
the file into a suitable directory. Note that the directories in the path for
the AGE2EDOT and RESPTIME programs must have names that are no longer than 8
characters in length. These programs will not run if the directory names
fail this specification. The programs are started by double -clicking
the file name. The programs require no input files. Rather, the user is
guided by a set of prompts and questions to supply the necessary input
parameters for the calculation of interest. Results are output to a window
for CLOSURE and to an output file for AGE2EDOT and RESPTIME. In all
cases, the output is organized with tab -separated columns, so that it can
be easily imported into a plotting program, such as EXCEL or
SIGMAPLOT. Upgrades will be posted at:
www.geology.yale.edu/~brandon.
The source code for the programs is available on request.

DISTRIBUTION
Files included in this distribution are:
Documentation.pdf Explanation of programs, including methods used, source of
data, etc.
Closure.exe Stand-alone windows-style program (error corrected, June, 2007)
Age2Edot.exe Stand-alone console-style program
RespTime.exe Stand-alone console-style program
Age2Edot.output Sample output file
Resptime.output Sample output file

REFERENCE
Brandon, M. T., Roden-Tice, M. K., and Garver, J. I., 1998, Late Cenozoic
exhumation of the Cascadia accretionary wedge in the Olympic Mountains,
northwest Washington State: Geological Society of America Bulletin, v. 110, p.
985-1009.

Ehlers, T., Chaudhri, T., Kumar, S., Fuller, C., Willett, S., Ketcham, R. A.,
Brandon, M. T., Belton, D. X., Kohn, B. P., Gleadow, A. J. W., Dunai, T. J.,
and Fu, F. Q., 2005, Computational tools for low-temperature thermochronometer
interpretation, in Reiners, P., and Ehlers, T., editors, Low-Temperature Thermochronology:
Techniques, Interpretations, Applications: Reviews in Mineralogy and Geochemistry: Chantilly,
VA, Mineralogical Society of America, Geochemical Society, p. 589-622.

Reiners, P. W., and Brandon Mark, T., 2006, Using thermochronology to understand orogenic
erosion: Annual Review of Earth and Planetary Sciences, v. 34, p. 419–66,
doi: 10.1146/annurev.earth.34.031405.125202.

Mark T. Brandon
Department of Geology and Geophysics
Yale University
P.O. Box 208109
New Haven, CT 06520-8109

Office Phone: (203) 432-3135 FAX Phone: (203) 432-3134

Web: www.geology.yale.edu/~brandon

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