Which rock type is best for radiometric dating

Which rock is best suited for radiometric dating quizlet

. a surface within a stack of sedimentary rocks marked by erosion or nondeposition. so carbon 14 is used to date materials that aren’t that old geologically, say in the tens of thousands of years, while potassium-argon dating can be used to determine the ages of much older materials, in the millions and billions year range. radiometric dating is also used to date archaeological materials, including ancient artifacts. the technique has potential applications for detailing the thermal history of a deposit. zircon also forms multiple crystal layers during metamorphic events, which each may record an isotopic age of the event.: radiometric datingconservation and restorationhidden categories: cs1 maint: multiple names: authors listwikipedia articles needing page number citations from september 2010use dmy dates from september 2010. ages of these oldest rocks still don't tell us how old the earth is, but they do establish a minimum age. line of evidence involves rocks from outside the earth--meteorites and moon rocks..    older rocks are not always found on the earth surface. the discovery gave scientists a tool for dating rocks that contain radioactive elements. the fourth, lead 204, is not the result of radioactive decay. the age is calculated from the slope of the isochron (line) and the original composition from the intercept of the isochron with the y-axis. radiometric dating and the geological time scale: circular reasoning or reliable tools?[13][17] however, construction of an isochron does not require information on the original compositions, using merely the present ratios of the parent and daughter isotopes to a standard isotope. the uranium content of the sample has to be known, but that can be determined by placing a plastic film over the polished slice of the material, and bombarding it with slow neutrons. rock a contains inclusions of rock b, which rock is oldest? but the most accurate forms of absolute age dating are radiometric methods.Which rock type is best for radiometric dating

Radiometric dating - Wikipedia

this causes induced fission of 235u, as opposed to the spontaneous fission of 238u. uranium is water-soluble, thorium and protactinium are not, and so they are selectively precipitated into ocean-floor sediments, from which their ratios are measured. these rates are usually expressed as the isotope's half-life--that is, the time it takes for one-half of the parent isotopes to decay. "precise 206pb/238u age determination on zircons by laser ablation microprobe-inductively coupled plasma-mass spectrometry using continuous linear ablation". over time, ionizing radiation is absorbed by mineral grains in sediments and archaeological materials such as quartz and potassium feldspar. carbon-14 is a radioactive isotope of carbon, with a half-life of 5,730 years,[25][26] (which is very short compared with the above isotopes) and decays into nitrogen. that’s because zircon is super tough – it resists weathering. dating has been carried out since 1905 when it was invented by ernest rutherford as a method by which one might determine the age of the earth. if a rock has been partially melted, or otherwise metamorphosed, that causes complications for radiometric (absolute) age dating as well. pretty obvious that the dike came after the rocks it cuts through, right? on the other hand, the half-life of the isotope potassium 40 as it decays to argon is 1. older rocks are not always found on the earth surface. at a certain temperature, the crystal structure has formed sufficiently to prevent diffusion of isotopes. because all parts of the solar system are thought to have formed at the same time (based on the solar nebula theory), the earth must be the same age as the moon and meteorites--that is, about 4. three of these isotopes (lead 206, 207, 208) result from radioactive decay of isotopes of thorium and uranium. radioactive potassium-40 is common in micas, feldspars, and hornblendes, though the closure temperature is fairly low in these materials, about 350 °c (mica) to 500 °c (hornblende). plants acquire it through photosynthesis, and animals acquire it from consumption of plants and other animals.

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Radiometric Dating ( Read ) | Earth Science | CK-12 Foundation

when a consistent 129xe/128xe ratio is observed across several consecutive temperature steps, it can be interpreted as corresponding to a time at which the sample stopped losing xenon./nd isochron plotted of samples [14] from the great dyke, zimbabwe. is age of the sample,D is number of atoms of the daughter isotope in the sample,D0 is number of atoms of the daughter isotope in the original composition,N is number of atoms of the parent isotope in the sample at time t (the present), given by n(t) = noe-λt, and. thus an igneous or metamorphic rock or melt, which is slowly cooling, does not begin to exhibit measurable radioactive decay until it cools below the closure temperature. for example, which is older, the bricks in a building or the building itself? of the following reflects the correct parent isotope to daughter isotope? krot(2002) dating the earliest solids in our solar system, hawai'i institute of geophysics and planetology http://www. the final decay product, lead-208 (208pb), is stable and can no longer undergo spontaneous radioactive decay. geologic principle is simply express as the “present is the key to the past”? most radioactive nuclides, the half-life depends solely on nuclear properties and is essentially a constant. reality, geologists tend to mix and match relative and absolute age dates to piece together a geologic history. mathematical expression that relates radioactive decay to geologic time is[12][15]. links hererelated changesupload filespecial pagespermanent linkpage informationwikidata itemcite this page.) for example, the element carbon, which always has six protons in its nucleus, has three isotopes: one with six neutrons in the nucleus, one with seven, and one with eight. rate of creation of carbon-14 appears to be roughly constant, as cross-checks of carbon-14 dating with other dating methods show it gives consistent results.العربيةбългарскиcatalàčeštinadeutschespañolفارسیfrançais한국어hrvatskibahasa indonesiaíslenskaitalianoעבריתlietuviųmagyarnederlands日本語norsknorsk nynorskpolskiportuguêsрусскийsimple englishslovenščinasrpskohrvatski / српскохрватскиbasa sundasvenskaதமிழ்türkçeукраїнськаاردوtiếng việt中文. concordia diagram as used in uranium–lead dating, with data from the pfunze belt, zimbabwe. GeoKansas--Geotopics--Age of the Earth

How do we know the ages of fossils and fossil-bearing rocks?

based on the rule of superposition, certain organisms clearly lived before others, during certain geologic times. correct order of time stratigraphic units from largest to smallest isa. by measuring the decay products of extinct radionuclides with a mass spectrometer and using isochronplots, it is possible to determine relative ages of different events in the early history of the solar system. in situ micro-beam analysis can be achieved via laser icp-ms or sims techniques. in these cases, usually the half-life of interest in radiometric dating is the longest one in the chain, which is the rate-limiting factor in the ultimate transformation of the radioactive nuclide into its stable daughter. some meteorites contain the four lead isotopes but no uranium or thorium parents. method works because some unstable (radioactive) isotopes of some elements decay at a known rate into daughter products. like the other kind of dating, geologic dating isn’t always simple. in many cases, the daughter nuclide itself is radioactive, resulting in a decay chain, eventually ending with the formation of a stable (nonradioactive) daughter nuclide; each step in such a chain is characterized by a distinct half-life. the narrower a range of time that an animal lived, the better it is as an index of a specific time. this in turn corresponds to a difference in age of closure in the early solar system. alternatively, if several different minerals can be dated from the same sample and are assumed to be formed by the same event and were in equilibrium with the reservoir when they formed, they should form an isochron. relatively short-range dating technique is based on the decay of uranium-234 into thorium-230, a substance with a half-life of about 80,000 years. unfortunately, none of the original rocks still exist, so scientists had to use less direct evidence to determine the age of the earth. some radioactive parent isotopes decay almost instantaneously into their stable daughter isotopes; others take billions of years. scientists assume that meteorites and moon rocks were not subjected to the extensive alteration that earth rocks have undergone.) to determine the relative ages of rocks or features such as faults.Geology 102 Final Exam Flashcards

Absolute dating and magnetostratigraphy

chart of a few different isotope half lifes: http://geomaps. (example search terms: “oldest rocks” “cretaceous-tertiary (kt) boundary” “native american fire ring” ). ma using lead–lead dating, results that are consistent with each other. the age that can be calculated by radiometric dating is thus the time at which the rock or mineral cooled to closure temperature. scientists can use radioactive decay to find the age of certain materials. is the most common unconformity but the most difficult to identify in the field. the temperature at which this happens is known as the closure temperature or blocking temperature and is specific to a particular material and isotopic system. thus, as an event marker of 1950s water in soil and ground water, 36cl is also useful for dating waters less than 50 years before the present. it is accompanied by a sister process, in which uranium-235 decays into protactinium-231, which has a half-life of 32,760 years.–lead dating is often performed on the mineral zircon (zrsio4), though it can be used on other materials, such as baddeleyite, as well as monazite (see: monazite geochronology). zircon has a very high closure temperature, is resistant to mechanical weathering and is very chemically inert. this can be seen in the concordia diagram, where the samples plot along an errorchron (straight line) which intersects the concordia curve at the age of the sample. rate of decay of radioactive isotopes strongly depends on temperature and pressure. radiometric dating generally requires that the parent has a long enough half-life that it will be present in significant amounts at the time of measurement (except as described below under "dating with short-lived extinct radionuclides"), the half-life of the parent is accurately known, and enough of the daughter product is produced to be accurately measured and distinguished from the initial amount of the daughter present in the material. of various rocks and minerals found in kansas, including mineral id tables and hardness scale. because the original abundances of lead on the planet cannot be measured, scientists use meteorites to get at the earth's original lead composition. this scheme is used to date old igneous and metamorphic rocks, and has also been used to date lunar samples.

Radiometric dating - Wikipedia

Radiometric Dating ( Read ) | Earth Science | CK-12 Foundation

Geologic Age Dating Explained - Kids Discover

36cl has seen use in other areas of the geological sciences, including dating ice and sediments. some isotopes are stable, but some are unstable or radioactive.[27] in other radiometric dating methods, the heavy parent isotopes were produced by nucleosynthesis in supernovas, meaning that any parent isotope with a short half-life should be extinct by now. plotting an isochron is used to solve the age equation graphically and calculate the age of the sample and the original composition.[8] precision is enhanced if measurements are taken on multiple samples from different locations of the rock body. rule is common sense, but it serves as a powerful reference point. for example, the age of the amitsoq gneisses from western greenland was determined to be 3..Use with this cross section of the grand canyon from the usgs’s teaching page: http://education. it is not affected by external factors such as temperature, pressure, chemical environment, or presence of a magnetic or electric field. oldest rocks dated on earth, which are younger than the absolute age of earth, are a. for rocks dating back to the beginning of the solar system, this requires extremely long-lived parent isotopes, making measurement of such rocks' exact ages imprecise. people, you can’t really guess the age of a rock from looking at it. another possibility is spontaneous fission into two or more nuclides. "the age and petrology of the chimbadzi hill intrusion, nw zimbabwe: first evidence for early paleoproterozoic magmatism in zimbabwe".–lead radiometric dating involves using uranium-235 or uranium-238 to date a substance's absolute age. type of rock best suited for radioactive dating is a. absolute age dating is like saying you are 15 years old and your grandfather is 77 years old.

How do we know the ages of fossils and fossil-bearing rocks?

Absolute dating and magnetostratigraphy


How do we know the Age of the Earth?

this transformation may be accomplished in a number of different ways, including alpha decay (emission of alpha particles) and beta decay (electron emission, positron emission, or electron capture). unconformity that exists between an igneous rocks and sedimentary rocks is defined as?.    a surface within a stack of sedimentary rocks marked by erosion or nondeposition. principles and applications of geochemistry: a comprehensive textbook for geology students (2nd ed. geologic age dating—assigning an age to materials—is an entire discipline of its own. is based on the beta decay of rubidium-87 to strontium-87, with a half-life of 50 billion years.[18] all the samples show loss of lead isotopes, but the intercept of the errorchron (straight line through the sample points) and the concordia (curve) shows the correct age of the rock. finally, correlation between different isotopic dating methods may be required to confirm the age of a sample. In a way, this field, called geochronology, is some of the purest detective work earth scientists do. scientists can use radioactive decay to find the age of certain materials. by allowing the establishment of geological timescales, it provides a significant source of information about the ages of fossils and the deduced rates of evolutionary change. in a way this field, called geochronology, is some of the purest detective work earth scientists do. the residence time of 36cl in the atmosphere is about 1 week. that corn cob found in an ancient native american fire pit is 1,000 years old. line of evidence is based on the present-day abundances of the various isotopes of lead found in the earth's crust. billion years for the earth, which is consistent with the ages determined from meteorites and lunar rocks.^ stewart, k,, turner, s, kelley, s, hawkesworh, c kristein, l and manotvani, m (1996).

Geologic Age Dating Explained - Kids Discover

Radiometric Dating: Methods, Uses & the Significance of Half-Life

the proportion of carbon-14 left when the remains of the organism are examined provides an indication of the time elapsed since its death. are two basic approaches: relative age dating, and absolute age dating. on extensive sampling of the earth's crust, scientists determined the present-day abundances of the four isotopes of lead relative to each other and to the parent isotopes that produced three of them. this makes carbon-14 an ideal dating method to date the age of bones or the remains of an organism. precision of a dating method depends in part on the half-life of the radioactive isotope involved. radiometric dating requires a measurable fraction of parent nucleus to remain in the sample rock. that is, at some point in time, an atom of such a nuclide will undergo radioactive decay and spontaneously transform into a different nuclide. example of short-lived extinct radionuclide dating is the 26al – 26mg chronometer, which can be used to estimate the relative ages of chondrules. the oldest rocks and soils from the moon are about the same age--4. the geologic time scale, what percentage of the rock history is covered by the precambrian period?[16] dating can now be performed on samples as small as a nanogram using a mass spectrometer. when an organism dies, it ceases to take in new carbon-14, and the existing isotope decays with a characteristic half-life (5730 years). half-life simply means the amount of time it takes for half of a remaining particular isotope to decay to a daughter product. determine the relative age of different rocks, geologists start with the assumption that unless something has happened, in a sequence of sedimentary rock layers, the newer rock layers will be on top of older ones. the dating is simply a question of finding the deviation from the natural abundance of 26mg (the product of 26al decay) in comparison with the ratio of the stable isotopes 27al/24mg. this scheme has been refined to the point that the error margin in dates of rocks can be as low as less than two million years in two-and-a-half billion years. it’s based either on fossils which are recognized to represent a particular interval of time, or on radioactive decay of specific isotopes.

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    Radioactive dating | Define Radioactive dating at

    this predictability allows the relative abundances of related nuclides to be used as a clock to measure the time from the incorporation of the original nuclides into a material to the present. a material that selectively rejects the daughter nuclide is heated, any daughter nuclides that have been accumulated over time will be lost through diffusion, setting the isotopic "clock" to zero. the fission tracks produced by this process are recorded in the plastic film. a related method is ionium–thorium dating, which measures the ratio of ionium (thorium-230) to thorium-232 in ocean sediment.’s more, if the whole rock is badly weathered, it will be hard to find an intact mineral grain containing radioactive isotopes. as the mineral cools, the crystal structure begins to form and diffusion of isotopes is less easy. stimulating these mineral grains using either light (optically stimulated luminescence or infrared stimulated luminescence dating) or heat (thermoluminescence dating) causes a luminescence signal to be emitted as the stored unstable electron energy is released, the intensity of which varies depending on the amount of radiation absorbed during burial and specific properties of the mineral. it is therefore essential to have as much information as possible about the material being dated and to check for possible signs of alteration.[12][13] dating of different minerals and/or isotope systems (with differing closure temperatures) within the same rock can therefore enable the tracking of the thermal history of the rock in question with time, and thus the history of metamorphic events may become known in detail. billion years, and so this method is applicable to the oldest rocks. carbon-14, though, is continuously created through collisions of neutrons generated by cosmic rays with nitrogen in the upper atmosphere and thus remains at a near-constant level on earth. the procedures used to isolate and analyze the parent and daughter nuclides must be precise and accurate. students work alone or in pairs to find an article or paper that uses radiometric age dating.. the rate of decay is constant for a particular element. of these is not a reason why earth rocks are younger than meteorites and moon rocks? equation is most conveniently expressed in terms of the measured quantity n(t) rather than the constant initial value no. in uranium–lead dating, the concordia diagram is used which also decreases the problem of nuclide loss.
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    Radiometric dating age of earth -

    is not as reliable a representation of truth as is a “scientific law.[1] the use of radiometric dating was first published in 1907 by bertram boltwood[2] and is now the principal source of information about the absolute age of rocks and other geological features, including the age of fossilized life forms or the age of the earth itself, and can also be used to date a wide range of natural and man-made materials. after irradiation, samples are heated in a series of steps and the xenon isotopic signature of the gas evolved in each step is analysed. the fall season approaches, snow begins to fall in the rocky mountains. by using this site, you agree to the terms of use and privacy policy. this means that as radioactive parent elements decay, they and their daughters are trapped together inside the crystal. of the parent/daughter radioactive isotopes used to date minerals has the shortest half-life and, therefore, is capable of dating the youngest geologic events? determined the earth's age using a technique called radiometric dating. on the other hand, the concentration of carbon-14 falls off so steeply that the age of relatively young remains can be determined precisely to within a few decades..So geochronolgists just measure the ratio of the remaining parent atom to the amount of daughter and voila, they know how long the molecule has been hanging out decaying. say for example that a volcanic dike, or a fault, cuts across several sedimentary layers, or maybe through another volcanic rock type. after an organism has been dead for 60,000 years, so little carbon-14 is left that accurate dating can not be established. "precise u–pb mineral ages, rb–sr and sm–nd systematics for the great dyke, zimbabwe—constraints on late archean events in the zimbabwe craton and limpopo belt".^ a b oberthür, t, davis, dw, blenkinsop, tg, hoehndorf, a (2002). the decay of thorium-232, what stable daughter isotope is produced? the possible confounding effects of contamination of parent and daughter isotopes have to be considered, as do the effects of any loss or gain of such isotopes since the sample was created. this means that the lead composition in these meteorites has not changed since their formation, and scientists believe this is a reasonable approximation of the composition of the earth's original lead, the so-called primordial lead.
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    Carbon-14, Radiometric Dating - CSI

    the amounts of the four lead isotopes in primordial lead to their present amounts, scientists can determine how much lead has been added by radioactive decay since the earth was formed. additionally, elements may exist in different isotopes, with each isotope of an element differing in the number of neutrons in the nucleus. amounts of otherwise rare 36cl (half-life ~300ky) were produced by irradiation of seawater during atmospheric detonations of nuclear weapons between 1952 and 1958. but if the hourglass were to break (become an open system), sand leaks out and the hourglass is no longer a reliable tool for telling time..    the rate of decay is constant for a particular element. also like this simple exercise, a spin-off from an activity described on the usgs site above. "a titanite fission track profile across the southeastern archæan kaapvaal craton and the mesoproterozoic natal metamorphic province, south africa: evidence for differential cryptic meso- to neoproterozoic tectonism". dating works best on igneous rocks, which are formed from the cooling of molten rock, or magma. is not as reliable a representation of truth as is a hypothesis. the mass spectrometer was invented in the 1940s and began to be used in radiometric dating in the 1950s. this temperature is what is known as closure temperature and represents the temperature below which the mineral is a closed system to isotopes. they can then calculate, using the half-life of each parent, how long it took to create the differences between the amount of present-day lead and primordial lead for each of the three isotopes..Have students reconstruct a simple geologic history — which are the oldest rocks shown? dating (absolute time dating) of mineral crystals depends on a. absolute age dating, you get a real age in actual years. geologist who proposed the principle of cross-cutting relationships and the principle of inclusions and was a strong supporter of the hypothesis (later theory) of uniformitarianism. a stack of sedimentary rocks that has not been deformed or overturned, the oldest rocks occur a.
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    Dating Methods | Answers in Genesis

    radiometric dating is based upon the fact that some forms of chemical elements are radioactive, which was discovered in 1896 by henri becquerel and his assistants, marie and pierre curie.” father of modern geology” who was a proponent of plutonism as one aspect of earth formation but is best remembered for proposing what is now the theory of uniformitarianism. here is an easy-to understand analogy for your students: relative age dating is like saying that your grandfather is older than you. geologist who served as an informal naturalist on the voyage of the hmv beagle and later wrote “origin of species by means of natural selection. isotopic systems that have been exploited for radiometric dating have half-lives ranging from only about 10 years (e. elements have naturally occurring isotopes, varieties of the element that have different numbers of neutrons in the nucleus. therefore, scientists perform radiometric dating only on rocks or minerals that have remained closed systems. dating methods based on extinct radionuclides can also be calibrated with the u-pb method to give absolute ages. cracks preserved in shale or mudrock can be used to determine “stratigraphic up” in an overturned sequence of sedimentary rocks.[3] among the best-known techniques are radiocarbon dating, potassium–argon dating and uranium–lead dating. rocks above the surface of the ground is described as?, 1989, historical geology--evolution of the earth and life through time: st. at any moment, the ratio between them is a measure of the time elapsed, as long as the system remains closed. hypothesis of hsu and ryan about the origin of evaporate rocks in the sediments below the mediterranean sea a. scientists have determined the parent-daughter ratio, they can use this measurement along with half-life of the parent to calculate the age of a rock containing the radioactive isotope. of various geology topics, ranging from earth's age to the state's mining history. this converts the only stable isotope of iodine (127i) into 128xe via neutron capture followed by beta decay (of 128i).
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    Alkali Metal Dating, Rb-Sr Dating Model: Radioactive Dating, Part 4

    of its great advantages is that any sample provides two clocks, one based on uranium-235's decay to lead-207 with a half-life of about 700 million years, and one based on uranium-238's decay to lead-206 with a half-life of about 4. geology professor who was an expert in mining geology and was a proponent of neptunism. dating methods are not radiometric dating methods in that they do not rely on abundances of isotopes to calculate age.[14][19] an error margin of 2–5% has been achieved on younger mesozoic rocks. methods of radiometric dating vary in the timescale over which they are accurate and the materials to which they can be applied. the rates of decay of various radioactive isotopes have been accurately measured in the laboratory and have been shown to be constant, even in extreme temperatures and pressures. a particular isotope of a particular element is called a nuclide. fission tacking dating techniques, one of these mineral is not used. principle states that in any sequence of undisturbed strata, the oldest layer is at the bottom, and successively younger layers are successively higher? ideally, the mineral crystals in igneous rocks form a closed system--nothing leaves or enters the crystal once it is formed. (the nucleus of an atom is made up of protons and neutrons. "approximation of terrestrial lead isotope evolution by a two-stage model". geologists draw on it and other basic principles (http://imnh. discussion: good overview as relates to the grand canyon:Http://www2. involves inspection of a polished slice of a material to determine the density of "track" markings left in it by the spontaneous fission of uranium-238 impurities.[29] because the fission tracks are healed by temperatures over about 200 °c the technique has limitations as well as benefits. with stratigraphic principles, radiometric dating methods are used in geochronology to establish the geologic time scale.
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    Dating Fossils in the Rocks - National Geographic Society

    geology, rocks and minerals, and places to visit in the state's physiographic regions (including pdf factsheets for downloading). above equation makes use of information on the composition of parent and daughter isotopes at the time the material being tested cooled below its closure temperature. for dates up to a few million years micas, tektites (glass fragments from volcanic eruptions), and meteorites are best used. rubidium-strontium dating is not as precise as the uranium-lead method, with errors of 30 to 50 million years for a 3-billion-year-old sample.Λ is the decay constant of the parent isotope, equal to the inverse of the radioactive half-life of the parent isotope[16] times the natural logarithm of 2. There are two basic approaches: relative geologic age dating, and absolute geologic age dating. older rocks may have been deeply buried under sedimentary rocks c. this means that all of the lead 204 on the earth has been around since the formation of the earth. we know the earth must be at least as old as any rock on it. wikipedia® is a registered trademark of the wikimedia foundation, inc. the method compares the abundance of a naturally occurring radioactive isotope within the material to the abundance of its decay products, which form at a known constant rate of decay. the moment in time at which a particular nucleus decays is unpredictable, a collection of atoms of a radioactive nuclide decays exponentially at a rate described by a parameter known as the half-life, usually given in units of years when discussing dating techniques. so to date those, geologists look for layers like volcanic ash that might be sandwiched between the sedimentary layers, and that tend to have radioactive elements. as magma cools, radioactive parent isotopes are separated from previously formed daughter isotopes by the crystallization process. time, radioactive isotopes change into stable isotopes by a process known as radioactive decay. "the ~2400-year cycle in atmospheric radiocarbon concentration: bispectrum of 14c data over the last 8000 years" (pdf). excess of 26mg (often designated 26mg* ) is found by comparing the 26mg/27mg ratio to that of other solar system materials.

How do we know the Age of the Earth?

which rock type is best for radiometric dating

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