See closure temperature on Wiktionary
{
"etymology_text": "Coined 1973 by Martin H. Dodson.",
"forms": [
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"form": "closure temperatures",
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"expansion": "closure temperature (plural closure temperatures)",
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"examples": [
{
"ref": "1990, C. M. R. Fowler, The Solid Earth, Cambridge University Press, page 199:",
"text": "The relationship between the closure temperature of a mineral and its cooling history can be put onto a more rigorous footing by the use of some thermodynamics.",
"type": "quote"
},
{
"ref": "2006, Jean Braun, Peter van der Beek, Geoffrey Batt, Quantitative Thermochronology, Cambridge University Press, page 23:",
"text": "Dodson (1973) introduced the term closure temperature, which he defined as the temperature of the thermochronological system at the time t#95;c corresponding to its apparent age (cf. Figure 2.1). The closure temperature, which by definition lies between the open-system and blocking temperatures, provides the simplest conceptual entity to which a thermochronological age can be related.",
"type": "quote"
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{
"text": "2020, Barbara A. Romanowicz, Seismic Tomography of the Earth's Mantle, David Alderton, Scott A. Elias (editors-in-chief), Encyclopedia of Geology, Volume 1, 2nd Edition, Academic Press, page 606,\nAs the closure temperature varies for every mineral and isotopic system, a system can be closed for one mineral at some temperature but open for another."
}
],
"glosses": [
"The temperature, of a mineral, etc., below which there is no significant diffusion of isotopes into the external environment; the temperature of said mineral at the time it was formed (as calculated by radiometric dating)."
],
"id": "en-closure_temperature-en-noun-htMUraZA",
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"raw_glosses": [
"(geology) The temperature, of a mineral, etc., below which there is no significant diffusion of isotopes into the external environment; the temperature of said mineral at the time it was formed (as calculated by radiometric dating)."
],
"synonyms": [
{
"word": "blocking temperature"
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"translations": [
{
"code": "fr",
"lang": "French",
"sense": "temperature below which no significant diffusion occurs",
"tags": [
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"word": "température de fermeture"
},
{
"code": "fr",
"lang": "French",
"sense": "temperature below which no significant diffusion occurs",
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"word": "température de blocage"
},
{
"code": "de",
"lang": "German",
"sense": "temperature below which no significant diffusion occurs",
"tags": [
"feminine"
],
"word": "Schließungstemperatur"
},
{
"code": "hu",
"lang": "Hungarian",
"sense": "temperature below which no significant diffusion occurs",
"word": "záródási hőmérséklet"
}
],
"wikipedia": [
"closure temperature"
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}
],
"word": "closure temperature"
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{
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"text": "The relationship between the closure temperature of a mineral and its cooling history can be put onto a more rigorous footing by the use of some thermodynamics.",
"type": "quote"
},
{
"ref": "2006, Jean Braun, Peter van der Beek, Geoffrey Batt, Quantitative Thermochronology, Cambridge University Press, page 23:",
"text": "Dodson (1973) introduced the term closure temperature, which he defined as the temperature of the thermochronological system at the time t#95;c corresponding to its apparent age (cf. Figure 2.1). The closure temperature, which by definition lies between the open-system and blocking temperatures, provides the simplest conceptual entity to which a thermochronological age can be related.",
"type": "quote"
},
{
"text": "2020, Barbara A. Romanowicz, Seismic Tomography of the Earth's Mantle, David Alderton, Scott A. Elias (editors-in-chief), Encyclopedia of Geology, Volume 1, 2nd Edition, Academic Press, page 606,\nAs the closure temperature varies for every mineral and isotopic system, a system can be closed for one mineral at some temperature but open for another."
}
],
"glosses": [
"The temperature, of a mineral, etc., below which there is no significant diffusion of isotopes into the external environment; the temperature of said mineral at the time it was formed (as calculated by radiometric dating)."
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"(geology) The temperature, of a mineral, etc., below which there is no significant diffusion of isotopes into the external environment; the temperature of said mineral at the time it was formed (as calculated by radiometric dating)."
],
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"word": "blocking temperature"
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"translations": [
{
"code": "fr",
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"sense": "temperature below which no significant diffusion occurs",
"tags": [
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"word": "température de fermeture"
},
{
"code": "fr",
"lang": "French",
"sense": "temperature below which no significant diffusion occurs",
"tags": [
"feminine"
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"word": "température de blocage"
},
{
"code": "de",
"lang": "German",
"sense": "temperature below which no significant diffusion occurs",
"tags": [
"feminine"
],
"word": "Schließungstemperatur"
},
{
"code": "hu",
"lang": "Hungarian",
"sense": "temperature below which no significant diffusion occurs",
"word": "záródási hőmérséklet"
}
],
"word": "closure temperature"
}
Download raw JSONL data for closure temperature meaning in All languages combined (3.3kB)
This page is a part of the kaikki.org machine-readable All languages combined dictionary. This dictionary is based on structured data extracted on 2025-01-13 from the enwiktionary dump dated 2025-01-01 using wiktextract (4ba5975 and 4ed51a5). The data shown on this site has been post-processed and various details (e.g., extra categories) removed, some information disambiguated, and additional data merged from other sources. See the raw data download page for the unprocessed wiktextract data.
If you use this data in academic research, please cite Tatu Ylonen: Wiktextract: Wiktionary as Machine-Readable Structured Data, Proceedings of the 13th Conference on Language Resources and Evaluation (LREC), pp. 1317-1325, Marseille, 20-25 June 2022. Linking to the relevant page(s) under https://kaikki.org would also be greatly appreciated.