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Statistics for Fission Track Analysis - CRC Press Book

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Two exceptions are fission track and luminescence dating, which make use of changes that happen to materials surrounding some isotopes in rocks. Uranium-thorium dating method * Radiocarbon dating method * Fission track dating method * Chlorine dating method * Luminescence dating methods. He sets out the theory of fission track dating and through numerical examples, or geochronological research, or in geological applications of statistics, you will.

Fission Track Laboratory

While exposures of Precambrian rocks are generally scarce on the Colorado Plateau, good outcrops of early-Mesoproterozoic granitoids and gneissic rocks can be found within the deep canyons of the Uncompahgre Plateau e. This distinctive canyon cuts across the plateau in a southwest-northeast direction and provides an excellent cross section of the basement.

A well-defined unconformity between the basement and upper Triassic red siltstone is evident. Subsequent depositions on the plateau are Triassic—Jurassic sandstones and siltstones, followed by alternating Cretaceous shales and sandstones. The youngest sediments still preserved today are remnants of the Cenomanian—Campanian Dakota Sandstone and Mancos Shale e.

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A latest Cretaceous—Cenozoic sedimentary record is missing on the Uncompahgre Plateau. Whether the missing section was never deposited on the Uncompahgre Plateau or has been removed by later erosion during one or several periods of Laramide or younger tectonic uplift and exhumation is still debated. A striking feature of the northern Uncompahgre Plateau is the Unaweep Canyon, which, somewhat mysteriously, is drained by two creeks Fig.

This unusual drainage pattern has received a lot of attention since it was first described in the late s Peale, ; Gannett, ; the most recent contributions are Aslan et al. Most observers agree that these creeks cannot alone be responsible for the incision of the Unaweep Canyon.

A graben structure Ute Creek graben; Fig. The prevailing hypothesis seems to be that the canyon originates from late Cenozoic fluvial erosion by the ancestral Gunnison River e. The height and unusual location of the Unaweep drainage divide have led researchers to believe that this abandonment may have been caused by relatively recent tectonic uplift of the Uncompahgre Plateau e.

However, despite a few younger Quaternary fault movements reported south of the canyon Kirkham and Rogers, ; McCalpin, there is no clear structural evidence supporting such a neotectonic uplift event. An alternative explanation is a late Cenozoic Pleistocene glacial incision of the canyon. This was inspired by the seemingly U-shaped profile of the Unaweep Canyon e. Based on glacial features of the inner gorge cut into the Precambrian basement, Cole and Young suggested a possible late Pleistocene alpine glaciation.

However, a geophysical survey showed that the bedrock profile is most likely V-shaped, and that the modern U-shape can be attributed to valley-fill sedimentation Oesleby, The discovery of some late Paleozoic palynomorphs in drilled sedimentary strata close to the bedrock contact led Soreghan et al. However, this hypothesis is rather controversial: Immediately to the west of the Uncompaghre Plateau are the shallow intrusions of the La Sal Mountains, which form one of several Paleogene laccolithic complexes within the Colorado Plateau.

Whereas Cenozoic volcanic centers are mostly located along the plateau boundaries, these classical laccolithic intrusions are located within more central parts of the plateau Fig.

Meaning of "fission-track dating" in the English dictionary

The La Sal Mountains, just 30—40 km west of the Uncompahgre Plateau, include 3 of the 15 laccolith clusters of the Colorado Plateau, emplaced at levels ranging between 1. Similar ages are also found within other laccolithic intrusions of the Henry and Abajo Mountains Sullivan et al. Some older, Paleocene—Eocene hornblende K-Ar ages of 63—41 Ma from all three intrusions have been interpreted as the result of incompletely outgassed xenocrysts and excess of 40Ar in hornblende Nelson et al.

Two thermochronological studies have been carried out in the Unaweep Canyon. Three AHe ages of 25—17 Ma and another age of 42 Ma were reported for the central part of the canyon, while two ages of 23 and 47 Ma were given for the southwestern part. A few zircon U-Th -He ages were also reported, but show a wide scatter, —34 Ma. Thermal history models of their AFT data suggest complete thermal resetting of the AFT system in the late Eocene to Oligocene and two periods of rapid cooling, the first in the late Oligocene—early Miocene and the second during the last 6—10 m.

A recent study by Aslan et al.

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Based on thermal history modeling for these two samples, Aslan et al. Samples collected from the Uncompahgre Plateau can be divided into three groups: Apatite and zircon separates were obtained using conventional magnetic and heavy liquid separation techniques; 18 samples yielded enough apatite and were analyzed by the AFT method. The apatites were embedded in epoxy and then ground and polished to reveal internal crystal surfaces.

Each sample was then covered with a mica detector. A kinetic stage was used to control the grain to mica matching Dumitru, Central fission track ages were calculated with the TrackKey software Dunkl,using the zeta calibration method Hurford and Green, Due to relatively low track densities, eight samples were irradiated with Cf to increase the number of etchable confined tracks. Single apatite crystals were hand-picked using binocular and petrographic microscopes.

Only euhedral grains with two terminations were selected, and the length and width of each crystal were recorded. To determine the 4He content, each individual grain was packed in a platinum capsule and the capsule with the enclosed crystal was degassed under high vacuum by heating with an infrared diode laser.


To ascertain a quantitative helium extraction, re-extraction was performed for every sample. To analyze the U, Th, and Sm contents, the platinum capsules were retrieved after He analysis and the apatites were dissolved in nitric acid. The dissolved crystals were spiked with calibrated Th and U solutions and analyzed by the isotope dilution method on a Perkin Elmer Elan DRC inductively coupled—mass spectrometer equipped with an APEX microflow nebulizer.

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Form-dependent alpha-ejection corrections FT corrections were applied to all raw AHe ages, following the procedures of Farley et al. The mount was then ground to approximately half the grain thickness and polished, and the zircons were documented by optical reflected and transmitted light and scanning electron microscopy secondary electrons and cathodoluminescence. Prior to analysis, the mount was coated with 8—10 nm of ultrapure gold. The analytical method follows that in Williams and Claesson Each spot was rastered with the primary beam for s and then analyzed during 6 scans following the isotope peak sequence Zr2O, Pb, Every peak of every scan was measured sequentially 10 times with the following total counting times per scan: The following calibrations were carried out: Most zircons show well-defined euhedral shapes with length: Internally, the zircons are dominated by oscillatory zoned domains Fig.

Some zircons have no detectable cores Fig. Many zircons, however, show clear core-rim relationships, with more complex and often diffuse zoning in the cores Fig. These cores generally appear to be rounded fragments of larger grains and are interpreted to be xenocrystic cores inherited from the source region of the melts. We analyzed 31 spots on 27 grains Table 1 ; 22 spots were located on oscillatory-zoned domains, 3 spots were on assumedly magmatic cores, and 6 were on xenocrystic cores.

The older of these zircon core ages are typical for the Yavapai province and have crystallization ages of 1. However, large — Ma plutons also occur within the Yavapai province Premo and Van Schmus, and could have provided grains with these ages.

The AFT ages range from With the exception of samples CR05, CR19, and CR20, all ages were significantly younger than depositional ages of the overlying sedimentary rocks. This indicates that a process other than sedimentary burial caused post-Cretaceous thermal annealing in these samples. In the following we discuss the AFT results with respect to four subareas Fig.

A very steep age-elevation trend is apparent, suggesting fast cooling and little or no thermal influence after crystallization. Confined track length measurements on samples CR11 and CR14 yielded mean track lengths of Dislocations and other crystal defects are abundant in the samples from the La Sal Mountains, making track counting difficult.

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The poor sample quality can explain some of the spread in ages. The mean age for all six samples is Unaweep Canyon Six samples were dated from the Unaweep Canyon. This suggests that the samples were thermally affected during the late Eocene to Oligocene regional-scale volcanism. The ages are increasing from the southwestern canyon entrance toward the center of the canyon Unaweep divide and decrease again toward northeast. This trend is probably an effect of changes in elevation.

Length measurements were performed on 4 of the 6 samples, with mean track lengths varying between Uncompahgre Plateau Three samples from outside of Unaweep Canyon, from the top of the basement of the Uncompahgre Plateau, just below the overlying sediments, gave Paleocene ages, showing only a small variation between Therefore, the late Eocene to Oligocene thermal event that reset all the samples from within the Unaweep Canyon apparently had little effect on the AFT ages on the top of the Uncompahgre Plateau.

The preserved sedimentary rocks on top of the sampled Precambrian basement are of Late Triassic to Late Cretaceous age Williams, ; Jamison and Stearns, The early Paleogene AFT ages thus indicate heating during Mesozoic burial and subsequent cooling during Laramide uplift and erosion. The mean confined track lengths range from Sample CR02, with an age of Length measurements were performed on all three samples, with mean track lengths ranging from Five single apatite grains from sample CR19 yielded ages between These ages overlap, within their uncertainties, with the AFT ages from the Unaweep Canyon and the crystallization age of the La Sal Mountains intrusion.

This indicates that the late Eocene to Oligocene thermal event is present in the samples from the top of the basement of the Uncompahgre Plateau and that temperatures were high enough to reset U-Th -He ages but not AFT ages. - Registered at

Sample CR05 yielded four slightly older ages ranging from The oldest age should be excluded because the apatite contained small inclusions reported during grain selectionand a higher He re-extract indicates that these might have influenced the He measurement.

The mean of the remaining three ages is Thermal History Modeling Thermal history models were created by using the HeFTy software Ketcham, with the annealing algorithm by Ketcham et al. The ending condition for each model was set to good paths. The Uncompahgre Plateau was fully buried by the Western Interior Seaway throughout Cretaceous time, but might have undergone sedimentation until Paleocene—Eocene time; this is evident from the stratigraphic record of the nearby Book Cliffs Gualtieri, Triassic—Cretaceous burial is implemented in the models as a series of boxes that the temperature paths must pass through.

These first three boxes blue boxes in Figs. Since neither the exact timing nor depths are known for the maximum burial, a large box was chosen to allow the models a lot of freedom.

A large box was also used for the following uplift because timing and the amount of associated cooling were to be determined by the modeling. The timing of reheating during the late Eocene to Oligocene magmatism is well known, but the temperatures reached during this event are not well constrained. Thus this reheating event was implemented as a narrow but high box to allow a lot of freedom in the temperature but not in the timing. Unaweep Canyon Unaweep Canyon sample CR07 was chosen for thermal history modeling because it yielded the highest number of tracks.

Due to the complete thermal overprint in the late Eocene to Oligocene, the earlier thermal histories have effectively been erased and cannot be constrained by thermochronological data. But how he could not for the life of him determine.

Radiocarbon dating also referred to as carbon dating or carbon dating is a method for determining the age of an object material by using the properties of radiocarbon, a radioactive isotope of carbon.

fission track dating applications facebook

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