(U-Th)/He Thermochronology Lab

This book is focused on the basics of applying thermochronology to geological and tectonic problems, with the emphasis on fission-track thermochronology. It is conceived for relatively new practitioners to thermochronology, as well as scientists experienced in the various methods. The book is structured in two parts. Part I is devoted to the fundamentals of the fission-track method, to its integration with other geochronologic methods, and to the basic principles of statistics for fission-track dating and sedimentology applied to detrital thermochronology. Part I also includes the historical development of the technique and thoughts on future directions. Part II is devoted to the geological interpretation of the thermochronologic record.

Staff Profile

UiB has the only thermochronology laboratory in Norway. The main course objective is to train graduate student in broad aspects of thermochronology, specifically in fission-track analysis, and to prepare them to conduct an individual MSc or PhD project in this field. The course is accompanied by a seminar series, in which course participant study and present thermochronological case studies, such as from Antarctica, the Andes, the Apennines, the Canadian Shield, the North Sea and Scandinavia, and others.

The reading list will be available within June 1st for the autumn semester and December 1st for the spring semester. The course will be evaluated by the students in accordance with the quality assurance system at UiB and the department. The Programme Committee is responsible for the content, structure and quality of the study programme and courses.

argon thermochronology, Zeitler et al. () examined U-Th/He dating of apatite with the expec- tation that helium diffusion should be rapid at relatively low.

Lawrence W. Snee, John F. Sutter, William C. Economic Geology ; 83 2 : — Muscovite samples with an age difference as small as 2. Statistics are even better for comparison of multiple samples from separate events; that is, a difference of 0.

The Method: Thermochronology

The signals from K-feldspar have provided multiple thermometers for thermochronological study. These two protocols were further applied to the samples from the Nujiang River valley and both explicitly demonstrated the thermal history of the samples. They are suitable for K-feldspar thermochronology study.

Fission-track (FT) thermochronology can be integrated with the U–Pb and (U–Th​)/He dating methods. All three radiometric dating methods can be applied to.

Geochronology and thermochronology on detrital material provides unique constraints on sedimentary provenance, depositional ages, and orogenic evolution of source terrains. Typically these ages correspond to crystallization and exhumation or eruption ages, and their combination can be used to more confidently resolve candidate source terrains, establish maximum depositional ages, and constrain the thermal histories of orogenic source regions.

We present examples from Mesozoic aeolian sandstones, both modern and Paleogene fluvial sediments, and active margin turbidite assemblages from the Cascadia and Kamchatka margins. Important results include the fact that detritus from ancient orogens may dominate sediments thousands of kilometers away, crustal melting and exhumation appear to be spatially-temporally decoupled in at least two orogens, and first-cycle volcanic zircons older than depositional age are surprisingly rare in most settings except in the continental interior.

In the case of the Kamchatkan, and possibly Olympic, turbidites, zircon He ages are partially reset. User Name Password Sign In. Abstract Geochronology and thermochronology on detrital material provides unique constraints on sedimentary provenance, depositional ages, and orogenic evolution of source terrains. This Article doi: Services Email this article to a colleague Alert me when this article is cited Alert me if a correction is posted Similar articles in this journal Similar articles in Web of Science Download to citation manager.

Google Scholar Articles by Reiners, P. Articles by Cowan, D. Search for related content.


Thermochronology is the study of the thermal evolution of a region of a planet. Thermochronologists use radiometric dating along with the closure temperatures that represent the temperature of the mineral being studied at the time given by the date recorded to understand the thermal history of a specific rock, mineral, or geologic unit. It is a subfield within geology , and is closely associated with geochronology.

Eva Enkelmann reserach group for thermochronology at the Geology Department Ryan Grieco and Kade Damant conduct apatite and zircon U-Th/He dating.

The Earth System Dynamics research group maintains several different laboratories used to quantify interactions between the lithosphere, atmosphere, and biosphere at the Earth’s surface. Interested parties should contact Todd Ehlers. Rock cooling histories can be significantly influenced by erosion and topography.

We use low-temperature thermochronology to quantify the deformation, erosion, and paleotopographic history of orogens. All facilities required for high-quality mineral separations are available in house. Leica and Olympus high-end stereo and cross-polarized binocular microscopes are available for sample preparation. Following sample preparation, apatite and zircon samples are degassed using a Patterson instruments extraction line with a diode laser and quadrupole mass spectrometer. The system is fully automated.

U, Th, and Sm are measured with an inductively coupled plasma mass spectrometer through collaborative partnerships. Furthermore, a Zeiss M2M microscope with Autoscan software was recently installed and used for standard and fully automated track counting. All facilities are ‘in house’ required for sample preparation grain mounts, polishing on a Struers Tegrapol system and etching.

We use the external dector method on apatite and zircon. Sample irradiations are done with thermal neutrons at the Garching reactor Munich. Cosmogenic isotopes are a powerful tool for quantifying erosion rates on time scales shorter , yr than thermochronometers are sensitive to.

Facilities & Equipment

There are many isotopes and minerals that can be used for radiometric dating and therefore many different ways to perform a thermochronology study. Toggle navigation. Search open E I. Other definitions: Wikipedia Reegle. The closure temperature is when the crystal structure of a mineral has formed and cooled sufficiently to prevent diffusion of isotopes. At this point the mineral begins to display measurable radioactive decay.

“Apatite triple dating and white mica 40Ar/39Ar thermochronology of syntectonic detritus in the Central Andes: A multiphase tectonothermal history,” Geology.

The lab manager supports user training, sample processing, equipment maintenance, and planning and design in both labs. The He dating lab at the UofA supports training and analyses for diverse projects and workshops involving both external and internal PIs, undergraduate and graduate students, postdocs, and faculty. The lab conducts research in tectonic and geomorphic applications and experimental development and innovative applications of He dating.

It performs experiments necessary for dating and interpreting He ages of unexplored phases, improved analytical methods, and applying He dating to a range of novel problems such as surface wildfire, detrital studies, and meteorite thermal histories. In addition to supporting He dating operations for both internal and external users, the technician support proposed here will provide for routine high-resolution sector ICP-MS analyses and training to a broad spectrum of users internal and external to the University of Arizona.

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Thermochronology and Continental Tectonics

We should attach importance to conservation and changes of ore deposits besides metallogenic environment, ore deposit model and origin research. The conservation is closely related to uplifting and denudation so that to recover histories of uplifting and denudation for ore districts could reveal conservation and changes of mineral deposits. By applying fission track thermochronology, this chapter presents a research sample to discuss the issue, especially the relative technical method, and provides evidences for both deep ore prospecting and mineralizing potentiality evaluation.

Meanwhile, dating mineralizing age is another frontier topic in the world. The author successfully applied fission track thermochronology to determining the mineralizing ages and epochs of the hydrothermal deposits.

Low temperature thermochronology from Knox Rift region de Laeter Centre (​Curtin University), using conventional single grain (U-Th)/He dating techniques.

Skip to Content. James Metcalf. This automated He extraction and analysis system, optimized for reliably charac- terizing small gas amounts, is the heart of the CU TRaIL. Samples are loaded into an ultra-high vacuum chamber with a sapphire viewport attached to an automated stage. The evolved gas is then spiked with isotopically pure 3 He, cleaned with active gettering systems, and finally analyzed with a Pfeiffer Balzers QME quadrupole mass spectrometer.

The Alphachron also has a diffusion cell capable of high-precision diffusion experiments used to better understand the He diffusion kinetics of different minerals. This instrument will be equipped with a sample-introduction system that can withstand concentrated hydrofluoric acid and will be optimized for measuring trace element and isotopic compositions of dissolved silicate minerals. Since opening in , the lab has generated thousands of analyses for internal and external projects, and hosts numerous visitors annually.

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Mark Harrison (UCLA) Thermochronology

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