Monazite geochronology

Monazite is a common accessory mineral in various metamorphic and magmatic rocks, and is widely used for U—Pb geochronology. However, linking monazite U—Pb ages with the PT evolution of the rock is not always straightforward. We investigated the behaviour of monazite in a metasedimentary sequence ranging from greenschist facies phyllites into upper amphibolites facies anatectic gneisses, which is exposed in the Eocene Chugach Metamorphic Complex of southern Alaska. We investigated textures, chemical compositions and U—Pb dates of monazite grains in samples of differing bulk rock composition and metamorphic grade, with particular focus on the relationship between monazite and other REE-bearing minerals such as allanite and xenotime. In the greenschist facies phyllites, detrital and metamorphic allanite is present, whereas monazite is absent. In anatectic gneisses, new low-Y, high-Th monazite Mnz2 crystallised from partial melts, and a third, high-Y, low-Th monazite generation Mnz3 formed during initial cooling and garnet resorption. This study documents polyphase, complex monazite growth and dissolution during a single, relatively short-lived metamorphic cycle.

Investigation of the monazite chemical dating technique

Skip to search form Skip to main content You are currently offline. Some features of the site may not work correctly. Representing diverse igneous and metamorphic lithologies, these grains yielded conventional isotopic ages ranging in age from Neoarchean to Devonian.

called “common” Pb), a number of other U-bearing minerals are amenable to U–​Pb dating (e.g., titanite, apatite, monazite, xenotime, rutile, baddeleyite.

Monazite is an underutilized mineral in U—Pb geochronological studies of crustal rocks. It occurs as an accessory mineral in a wide variety of rocks, including granite, pegmatite, felsic volcanic ash, felsic gneiss, pelitic schist and gneiss of medium to high metamorphic grade, and low-grade metasedimentary rocks, and as a detrital mineral in clastic and metaclastic sediments.

In geochronological applications, it can be used to date the crystallization of igneous rocks, determine the age of metamorphism in metamorphic rocks of variable metamorphic grade, and determine the age and neodymium isotopic characteristics of source materials of both igneous and sedimentary rocks. It is particularly useful in the dating of peraluminous granitic rocks where zircon inheritance often precludes a precise U—Pb age for magmatic zircon.

The U—Pb systematics of the mineral are not without complexity, however. Being a mineral that favors incorporation of Th relative to U, it can contain considerable amounts of excess Pb derived from initially incorporated Th, an intermediate decay product of U. Monazite is known to be capable of preserving inheritance in a manner similar to that of zircon, and it can lose Pb during episodic or prolonged heating events of uppermost amphibolite and granulite facies metamorphic grades.

Examples of U—Pb systematics from most of the above situations are presented in this paper to illustrate both the utility and complexity of monazite in geochronological studies in an attempt to encourage more widespread application of this dating method. Nadia Mohammadi , Christopher R. McFarlane , David R. Lentz , Kathleen G. Jean-Pierre Burg , Pierre Bouilhol. Andrew DuFrane. Alcock , P.

Canadian Journal of Earth Sciences

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Monazite dating; CGGC; P–T condition; Rodinia assembly. 1. Introduction. Electron micro probe analyser (EPMA) monazite dating has been extensively used for.

All publications more feeds DOI: BibTeX file. Electron microprobe dating of monazite was performed on enclaves of sapphirine-bearing granulites and their host granites from the southeastern part of the Madurai Block in India. The granulites are strongly migmatitic and comprise quartzofeldspathic leucosome veins and restitic domains of sapphirine, garnet, orthopyroxene, sillimanite and cordierite. Inclusions of sapphirine-quartz intergrowths in garnet testify to an UHT stage of metamorphism which was followed by a stage of decompression during which garnet was replaced by coronitic opx-sill intergrowths.

Monazite inclusions in garnet, orthopyroxene and quartz often yield a bimodal age distribution of Mid- to early Neoproterozoic Ma ages in the cores which are rimmed by late Neoproterozoic age domains Ma. Monazites in the granite and the charnockite exclusively yield Pan-African values. The occurrence of sapphirine-quartz intergrowths and the early Neoproterozoic age population in the same petrographical position infers that the crystalline basement of the Madurai Block already experienced a stage of UHT metamorphism prior to the Pan-African orogenic event.

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Dating xenotime

Hacker, M. Racek, R. Holder, A.

Numerous techniques have been published for dating monazite including isotope dilution measurements using thermal ionization mass.

Monazite is a light rare earth element LREE -bearing phosphate mineral. Crystals typically contain distinct chemical domains, each of which represent successive growth thru geologic history. Electron microprobe analysis can characterize the geometry and U-Th- total Pb age for each domain. This kind of data allow the growth of monazite to be related to geologic events affecting the host rock. Monazite is common in pelitic and psammitic metamorphic rocks at greenschist facies and above where it is often recognized as inclusions in porphyroblasts but may also be in direct connection with the matrix.

Locating monazite grains can be done on standard geological thin sections via x-ray compositional mapping.

(U-Th)/He Dating of Phosphates: Apatite, Monazite, and Xenotime

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Monazite is common in sediments and sedimentary rocks (e.g., Kapoor et al. monazite dating has proliferated perhaps due to developments in a variety of.

Farley, Kenneth A. Reviews in Mineralogy and Geochemistry. ISBN Full text is not posted in this repository. Consult Related URLs below. For example, apatite usually has a few tens of ppm of both U and Th, while monazite and xenotime usually have hundreds of ppm to weight percent levels of these elements.

Molten element ark

Monazite rim formation was facilitated via dissolution-reprecipitation of Neoproterozoic monazite. The monazite rims record garnet growth as they are depleted in Y2O3 with respect to the Neoproterozoic cores. Rims are also characterized by relatively high SrO with respect to the cores. Results of the zircon depth-profiling revealed igneous zircon cores with crystallization ages typical for SNC metasediments.

These results show that both monazite and zircon experienced dissolution-reprecipitation under high-pressure conditions.

Abstract. Monazite laser ablation–split-stream inductively coupled plasma–mass spectrometry (LASS) was used to date monazite in situ in.

Molten element ark. If there seem to be no signs of damage and the element continues to spark even when plugged into a different socket on the stove, it is most likely defective and should be replaced. A there is NOT a chemical reaction B there is a change at the molecular level C atoms are spread apart D electrical charges are involved Rare Earth Element Production: This chart shows a history of rare earth element production, in metric tons of rare earth oxide equivalent, between and A rock is an aggregate of one or more minerals, or a body of undifferentiated Shop a wide selection of Fishing Gear in the Amazon.

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Petrology and monazite dating of the Fe-rich gneisses from Kokava Veporic Unit, Western Carpathians, Slovakia : Devonian sediments supplied from Gondwanan-sources metamorphosed in the Variscan times. Journal of Geosciences, volume 56 , issue 2 , – Geol Carpath Geol Zbor Geol Carpath Eclogae Geol Helv

Monazite is common in pelitic and psammitic metamorphic rocks at greenschist Dating monazite follows the U-Th total Pb age method which is described.

Colin A. Shaw, Karl E. Karlstrom, Michael L. Williams, Michael J. Jercinovic, Annie M. McCoy; Electron-microprobe monazite dating of ca. Geology ; 29 8 : — The Homestake shear zone, one of the principal Precambrian structures within the Colorado mineral belt, has a history of tectonism that extends from the Proterozoic to the Tertiary.

Electron Microprobe Dating of Monazite

Polygenetic monazite grains in diverse Precambrian crystalline rocks from the Black Hills, South Dakota, have been analyzed in situ by ion and electron microprobe methods SHRIMP and EMP , to evaluate the accuracy and precision of EMP ages determined using a new analytical protocol that incorporates improved background acquisition and interference corrections.

The monazite data set includes EMP chemical analyses from 26 grains in six metamorphic rocks, which resolve into 54 age-composition domains, and 31 SHRIMP isotopic ages from 13 grains in one of the rocks, with six grains microanalyzed in common by the two methods. The data set also includes monazite-bearing garnets in two of the rocks, whose isotopic compositions were analyzed using Pb stepwise-leaching PbSL methods.

The monazite grains selected for dating in these rocks tend to appear as equant or elongate grains reflecting end section and prismatic orientations, respectively​.

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Here, we analyse reference materials by atom probe tomography and develop a protocol for Pb/Th dating of nanoscale domains of monazite (

Geological Survey Distributor : U. Toggle navigation ScienceBase-Catalog. Your browser does not have support for cookies enabled. Some features of this application will not work. Publication Date Time Period Moscati, R. Samples in the form of mounted loose grains were prepared and analyzed for direct age dating on a laser ablation inductively coupled plasma mass spectrometer LA-ICPMS system at the U.

Geological Survey in Denver, Colorado in February

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