Time resolved rutile U/Pb data derived from LA-ICPMS – a case study from the North Pamir

Box , Beijing , P. E-mail: xieliewen mail. The advantages include high spatial resolution, high sample throughput, good precision and accuracy, and limited sample preparation. For the application of these techniques in U—Th—Pb geochronology, the main challenges involve ion counter drift, matrix differences between reference materials and samples, laser-induced downhole elemental fractionation and common lead corrections. We review recent efforts to improve spatial resolution, calibrate ion counter drift, and correct for common lead contamination, elemental fractionation and matrix mismatching. Multi-collectors simultaneously measure all isotopic signals over flat-topped peaks so that 1 the detection efficiency is significantly improved and relatively high spatial resolution is obtained, 4,5 and 2 the effects of spectral skew and flicker noise from the plasma source or ablated particles are removed or significantly reduced, resulting in improved counting statistics and lower internal and external uncertainties in isotopic ratios. The coupling of laser systems and more than one MS system where the carrier gas flow and, therefore, the ablated product is split between the mass spectrometers has been termed laser ablation split stream LASS analysis.

Closure temperature

This study investigates Ti mobility in the presence of halogens, as shown by the hydrothermal alteration of magmatic rutile in syenite. The syenite pegmatite studied intrudes gabbro, is preserved as a tectonic block in a major strike-slip fault zone, and formed in a back-arc environment in which there was widespread A-type granite plutonism. Magmatic rutile in the syenite forms millimetric-scale crystals rimmed by magmatic titanite and magnetite and also occurs as smaller interstitial crystals.

The syenite was synchronous with the later phases of regional A-type granite plutonism. Later hydrothermal halogen-rich fluids, derived from dissolution of halite, produced widespread metasomatic scapolite in the syenite.

A growing body of research focusing on U-Pb dating of rutile by LA ICP-MS is greatly improving our understanding of the behavior of this mineral with regards to.

Sovereign has identified a potentially globally significant, strategic rutile province across its large Malawi ground holding. The Malawi Rutile Province features two confirmed, discrete rutile mineralisation styles hosted respectively in sand and saprolite soft, friable weathered material which are both amenable to conventional processing. Rutile mineralisation identified to date has generally not been spatially constrained by drilling at either of the two main prospects, Kasiya saprolite and the Bua Channel sand.

The Company is targeting large resources that could support long-life, large-scale rutile production. The mineralised zone continues to be open along strike in both directions and open laterally to the south east. All mineralisation occurs from surface and is hosted in soft, free-dig, friable saprolite. A large percentage of intercepts remain open at depth with high-grade rutile mineralisation interpreted to extend to the base of the soft saprolite at around 25m.

Metallurgical test-work with saprolite material has demonstrated that very high-quality rutile meeting or exceeding typical market specifications can be produced. The Malawi Rutile Province features two confirmed, discrete rutile mineralisation styles; residual saprolite which is soft, friable weathered material i. Kasiya and traditional placer sand i. Bua Channel.

Geochemical and geochronological dataset of rutile from a Variscan metabasite in Sardinia, Italy

Email address:. Rutile dating. Laser-Ablation split-stream lass analysis in situ trace element, we will test rutile and zircon from approximately — Title trace element systematics in situ trace elements. Sims technique for rutile dating is an o.

High-sensitivity U–Pb rutile dating by secondary ion mass spectrometry (SIMS) with an O2. + primary beam. Axel K. Schmitt a,⁎, Thomas Zack b,1 a Department​.

Read the full text on a web page. U—Pb age data collected from detrital rutile and zircon in these rocks indicates these sequences contain very similar age spectra, although with a notable and important shift to younger ages within the stratigraphically younger Reynolds Range Group. Detrital rutile from the same rock yield a unimodal age spectrum with a mean age of ca.

The detrital zircon age spectrum from the Reynolds Range Group is similar, although the youngest cluster of ages is younger and dates to between Ma and Ma. Detrital rutile from these rocks yield a unimodal age spectrum with a mean age of ca. Although the observed differences in ages are subtle, we suggest these nevertheless mark a significant change in provenance.

This orogenic belt marks collision between the North Australian and Kimberley cratons, an event dated to between Ma and Ma and which incorporates marginally older rocks dating to Ma from the foreland of the Kimberley Craton. By contrast we attribute the influx of younger rutile and zircon, together with a distinct facies change observed with the onset of the deposition of the Reynolds Range Group, to a shift in provenance region to the Yapungku Orogen, which marks the collision between the West Australian and North Australian cratons and is dated to ca.

A change in provenance is additionally consistent with significant differences in rutile trace element composition. We suggest this indicates spatially continuous basinal conditions within the North Australian Craton between ca. Tell a friend about this page Print version. The University of Gothenburg uses cookies to provide you with the best possible user experience. By continuing on this website, you approve of our use of cookies.

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Delia Rösel

Rutile is a common accessory mineral that occurs in a wide spectrum of metamorphic rocks, such as in blueschists, eclogites, and granulites and as one of the most stable detrital heavy minerals in sedimentary rocks. The advent of rutile trace element thermometry has generated increased interest in a better understanding of rutile formation. Rutile thermometry of the same detrital grains indicates former granulite-facies conditions.

The methods outlined in this paper should find wide application in studies that require age information of single spots, e. This is a preview of subscription content, log in to check access.

with ≥ 40 ppm Hf. A new rutile standard for in situ U-Pb dating, Wodgina, has been characterised by SHRIMP, TIMS and limited LA-ICPMS.

Reviews in Mineralogy and Geochemistry ; 83 1 : — Rutile TiO 2 is an important accessory mineral that, when present, offers a rich source of information about the rock units in which it is incorporated. It occurs in a variety of specific microstructural settings, contains significant amounts of several trace elements and is one of the classical minerals used for U—Pb age determination. Here, we focus on information obtainable from rutile in its original textural context. We do not present an exhaustive review on detrital rutile in clastic sediments, but note that an understanding of the petrochronology of rutile in its source rocks will aid interpretation of data Shibboleth Sign In.

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In situ U-Pb rutile dating by LA-ICP-MS

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Most absolute dating methods rely on the analysis of radioactive isotopes and titanite, rutile, monazite and xenotime can be used to date high temperature.

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Rutile U-Pb Geochronology

We implement several procedures that help combat these analytical issues. Pb and U. To decrease molecular interferences at Pb peaks and increase the signal:noise ratio, we also use the energy filter to only accept high-energy ions into the collector. Because common lead and the amount of molecular interferences vary by sample, energy filtering is not always used.

Details. Description: Rutile Ore. Lot: N/A. Expiration Date: Unit Price *: $ Unit of Issue: 90 g. Status: Now Selling. Certificate Date: 1/22/ MSDS Date.

Chemical analyses show that rutile included in other minerals Rt inc commonly show higher SiO 2 and FeO contents and lower Nb 2 O 3 and ZrO 2 contents if compared with rutile in the matrix of the garnet-rich layer Rt mat. Cr 2 O 3 concentrations are quite similar in both types of rutile. Rt mat commonly shows a greater variability in minor elements, especially Nb 2 O 3 0. Few compilations of geochemical and geochronological data on rutile in Variscan metabasites can be found in literature, thus these data represent a new insight on a mineral phase the significance and scientific interest of which are rising in the last years.

Future studies on the origin and ages of emplacement and metamorphism either prograde or retrograde of this kind of rock, widespread in the Variscan chain, will benefit from these data as a term of comparison. Part of these data mainly Rt inc belongs to the supplementary material of [1].

Material Details

This paper presents new data related to the emplacement ages of the Amakinskaya and Taezhnaya kimberlites of the Mirny field, Siberia, located in the southern part of the Yakutian diamondiferous province. This study analyzed rutile and titanite grains along with zircons for U-Pb isotope composition by laser ablation LA -inductively coupled plasma-mass spectrometry ICP-MS and evaluated the applicability of rutile and titanite for the dating of kimberlite emplacements. Both minerals contain substantial admixtures of common Pb in their Pb isotope composition.

Therefore, the Pb method was applied for common Pb correction during age calculation.

microbeam U‐Pb dating and Hf isotopic determination. This study introduces the RMJG rutile as a new potential reference material, which.

A common oxide mineral is rutile TiO2 , which is present as an accessory mineral in many magmatic rocks and also occurs widely in high-grade metamorphic rocks, especially in blueschists, eclogites, and granulites. The scientific results and methodologies developed during our study will be disseminated to the geosciences community through publication of research papers and presentations at international meetings. Some full text articles may not yet be available without a charge during the embargo administrative interval.

Some links on this page may take you to non-federal websites. Their policies may differ from this site. Blackburn T. Kennedy, Donald J. DePaolo, John N. Christensen, and Ian Hutcheon [Earth Planet. Stockli, D. Blackburn, T. Wolfe, M. Zack, T.

Geochronology is the science of providing ages of events in the history of the Earth and extraterrestrial material and of determining the temporal rates of geological processes by using a number of different dating methods. The ages can be absolute e. Most absolute dating methods rely on the analysis of radioactive isotopes and their radiogenic decay products.

Similar conditions were used for U-Pb dating of rutile, using primary.

Stockli, George L. Luvizotto, Matthias G. Barth, Elena Belousova , Melissa R. Wolfe, Richard W. Rutile is a common accessory mineral that occurs in a wide spectrum of metamorphic rocks, such as in blueschists, eclogites, and granulites and as one of the most stable detrital heavy minerals in sedimentary rocks. The advent of rutile trace element thermometry has generated increased interest in a better understanding of rutile formation.

Rutile thermometry of the same detrital grains indicates former granulite-facies conditions. The methods outlined in this paper should find wide application in studies that require age information of single spots, e. N2 – Rutile is a common accessory mineral that occurs in a wide spectrum of metamorphic rocks, such as in blueschists, eclogites, and granulites and as one of the most stable detrital heavy minerals in sedimentary rocks.

AB – Rutile is a common accessory mineral that occurs in a wide spectrum of metamorphic rocks, such as in blueschists, eclogites, and granulites and as one of the most stable detrital heavy minerals in sedimentary rocks. Overview Fingerprint.

In radiometric dating , closure temperature or blocking temperature refers to the temperature of a system, such as a mineral , at the time given by its radiometric date. In physical terms, the closure temperature is the temperature at which a system has cooled so that there is no longer any significant diffusion of the parent or daughter isotopes out of the system and into the external environment.

Dodson ,"Closure temperature in cooling geochronological and petrological systems” in the journal Contributions to Mineralogy and Petrology , , with refinements to a usable experimental formulation by other scientists in later years.

Research——RMJG Rutile: A New Natural Reference Material for Microbeam U‐Pb Dating and Hf Isotopic Analysis,Le Zhang; Jia‐Lin Wu;.

Geosciences, 9 11 , doi The significant and continuous improvement of instrumentation and approaches has opened new fields of applications by extending the range of minerals that can be dated by this method. Following the development and distribution to the community of good quality reference materials in the last decade, rutile U-Pb thermochronology with a precision only slightly worse than zircon has become a commonly used method to track cooling of deep-seated rocks.

Recrystallization and secondary growth during metamorphism and the presence of grain boundary fluids can also affect the U-Pb isotopic system in rutile. A growing body of research focusing on U-Pb dating of rutile by LA ICP-MS is greatly improving our understanding of the behavior of this mineral with regards to retention of radiogenic Pb. This is key to fully exploit its potential as a tracker of geological processes.

The latest developments in this field are reviewed in this contribution.

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