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Lutetium–hafnium dating

Index Lutetium–hafnium dating

Lutetium–hafnium dating is a geochronological dating method utilizing the radioactive decay system of lutetium–176 to hafnium–176. [1]

40 relations: A-type granite, Baddeleyite, Chondrite, Chondritic uniform reservoir, Cumulate rock, Eclogite, Formation and evolution of the Solar System, Garnet, Geochronology, Goldschmidt classification, Hafnium, Half-life, Igneous rock, Incompatible element, Inductively coupled plasma mass spectrometry, Ionic radius, Isochron dating, Kyanite, Laurentia, Lutetium, Mass spectrometry, Metamorphic rock, Metamorphism, Petrogenesis, Phosphate minerals, Planetesimal, Pressure-temperature-time path, Protolith, Provenance (geology), Pyroxene, Radioactive decay, Rare-earth element, Refractory (planetary science), Thermal ionization mass spectrometry, Trace element, Valence (chemistry), Ytterbium, Zircon, Zirconium, Zirkelite.

A-type granite

A-type granites are a class of granite.

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Baddeleyite

Baddeleyite is a rare zirconium oxide mineral (ZrO2 or zirconia), occurring in a variety of monoclinic prismatic crystal forms.

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Chondrite

Chondrites are stony (non-metallic) meteorites that have not been modified due to melting or differentiation of the parent body.

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Chondritic uniform reservoir

The CHondritic Uniform Reservoir or CHUR is a scientific model in astrophysics and geochemistry for the mean chemical composition of the part of the Solar Nebula from which, during the formation of the Solar System, chondrites formed.

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Cumulate rock

Cumulate rocks are igneous rocks formed by the accumulation of crystals from a magma either by settling or floating.

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Eclogite

Eclogite is a mafic metamorphic rock.

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Formation and evolution of the Solar System

The formation and evolution of the Solar System began 4.6 billion years ago with the gravitational collapse of a small part of a giant molecular cloud.

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Garnet

Garnets are a group of silicate minerals that have been used since the Bronze Age as gemstones and abrasives.

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Geochronology

Geochronology is the science of determining the age of rocks, fossils, and sediments using signatures inherent in the rocks themselves.

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Goldschmidt classification

The Goldschmidt classification, developed by Victor Goldschmidt (1888-1947), is a geochemical classification which groups the chemical elements within the Earth according to their preferred host phases into lithophile (rock-loving), siderophile (iron-loving), chalcophile (ore-loving or chalcogen-loving), and atmophile (gas-loving) or volatile (the element, or a compound in which it occurs, is liquid or gaseous at ambient surface conditions).

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Hafnium

Hafnium is a chemical element with symbol Hf and atomic number 72.

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Half-life

Half-life (symbol t1⁄2) is the time required for a quantity to reduce to half its initial value.

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Igneous rock

Igneous rock (derived from the Latin word ignis meaning fire), or magmatic rock, is one of the three main rock types, the others being sedimentary and metamorphic.

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Incompatible element

In petrology and geochemistry, an incompatible element is one that is unsuitable in size and/or charge to the cation sites of the minerals of which it is included.

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Inductively coupled plasma mass spectrometry

Inductively coupled plasma mass spectrometry (ICP-MS) is a type of mass spectrometry which is capable of detecting metals and several non-metals at concentrations as low as one part in 1015 (part per quadrillion, ppq) on non-interfered low-background isotopes.

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Ionic radius

Ionic radius, rion, is the radius of an atom's ion in ionic crystals structure.

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Isochron dating

Isochron dating is a common technique of radiometric dating and is applied to date certain events, such as crystallization, metamorphism, shock events, and differentiation of precursor melts, in the history of rocks.

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Kyanite

Kyanite is a typically blue silicate mineral, commonly found in aluminium-rich metamorphic pegmatites and/or sedimentary rock.

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Laurentia

Laurentia or the North American Craton is a large continental craton that forms the ancient geological core of the North American continent.

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Lutetium

Lutetium is a chemical element with symbol Lu and atomic number 71.

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Mass spectrometry

Mass spectrometry (MS) is an analytical technique that ionizes chemical species and sorts the ions based on their mass-to-charge ratio.

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Metamorphic rock

Metamorphic rocks arise from the transformation of existing rock types, in a process called metamorphism, which means "change in form".

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Metamorphism

Metamorphism is the change of minerals or geologic texture (distinct arrangement of minerals) in pre-existing rocks (protoliths), without the protolith melting into liquid magma (a solid-state change).

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Petrogenesis

Petrogenesis, also known as petrogeny, is a branch of petrology dealing with the origin and formation of rocks.

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Phosphate minerals

Phosphate minerals are those minerals that contain the tetrahedrally coordinated phosphate (PO43−) anion along with the freely substituting arsenate (AsO43−) and vanadate (VO43−).

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Planetesimal

Planetesimals are solid objects thought to exist in protoplanetary disks and in debris disks.

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Pressure-temperature-time path

The Pressure-Temperature-time path (P-T-t path) is a record of the pressure and temperature (P-T) conditions that a rock experienced in a metamorphic cycle from burial and heating to uplift and exhumation to the surface.

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Protolith

A protolith is the original, unmetamorphosed rock from which a given metamorphic rock is formed (proto-: first; lithos: rock; both Greek).

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Provenance (geology)

Provenance in geology, is the reconstruction of the origin of sediments.

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Pyroxene

The pyroxenes (commonly abbreviated to Px) are a group of important rock-forming inosilicate minerals found in many igneous and metamorphic rocks.

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Radioactive decay

Radioactive decay (also known as nuclear decay or radioactivity) is the process by which an unstable atomic nucleus loses energy (in terms of mass in its rest frame) by emitting radiation, such as an alpha particle, beta particle with neutrino or only a neutrino in the case of electron capture, gamma ray, or electron in the case of internal conversion.

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Rare-earth element

A rare-earth element (REE) or rare-earth metal (REM), as defined by IUPAC, is one of a set of seventeen chemical elements in the periodic table, specifically the fifteen lanthanides, as well as scandium and yttrium.

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Refractory (planetary science)

In planetary science, any material that has a relatively high equilibrium condensation temperature is called refractory.

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Thermal ionization mass spectrometry

Thermal ionization mass spectrometry (TIMS) is a highly sensitive isotope mass spectrometry characterization technique that exploits the thermal ionization effect, in which a chemically purified sample is heated to cause ionization of the atoms of the sample.

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Trace element

A trace element is a chemical element whose concentration (or other measure of amount) is very low (a "trace amount").

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Valence (chemistry)

In chemistry, the valence or valency of an element is a measure of its combining power with other atoms when it forms chemical compounds or molecules.

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Ytterbium

Ytterbium is a chemical element with symbol Yb and atomic number 70.

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Zircon

Zircon is a mineral belonging to the group of nesosilicates.

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Zirconium

Zirconium is a chemical element with symbol Zr and atomic number 40.

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Zirkelite

Zirkelite is an oxide mineral with formula: (Ca,Th,Ce)Zr(Ti,Nb)2O7.

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Redirects here:

Lu-Hf dating, Lutetium-hafnium, Lutetium-hafnium dating.

References

[1] https://en.wikipedia.org/wiki/Lutetium–hafnium_dating

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