전문 번역가, 번역 회사, 웹 페이지 및 자유롭게 사용할 수 있는 번역 저장소 등을 활용합니다.
"a geologic time scale 2004" (cambridge university press).
"a geologic time scale 2004" (cambridge university press).
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") (2005) "a geologic time scale 2004" cambridge university press, cambridge, uk, isbn 0-521-78142-6.
") (2005) "a geologic time scale 2004" cambridge university press, cambridge, uk, isbn 0-521-78142-6.
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moreover, the radiation centers must be stable on geologic time, i.e., to have a very large lifetime, to make dating possible.
moreover, the radiation centers must be stable on geologic time, i.e., to have a very large lifetime, to make dating possible.
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while molecular dynamic simulation are very successful in predicting pico to nano second motions, they are often limited in their abilities in investigating "long"-time scale motions.
while molecular dynamic simulation are very successful in predicting pico to nano second motions, they are often limited in their abilities in investigating "long"-time scale motions.
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it also provides information about the dynamics in molecules on time scales slower than nanoseconds.
it also provides information about the dynamics in molecules on time scales slower than nanoseconds.
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most notabl is the fact that carbonates have a lower energy state than co2, which is why mineral carbonation is thermodynamically favorable and occurs naturally (e.g., the weathering of rock over geologic time periods).
most notabl is the fact that carbonates have a lower energy state than , which is why mineral carbonation is thermodynamically favorable and occurs naturally (e.g., the weathering of rock over geologic time periods).
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* demets, c., gordon, r., argus, d., stein, s., 1994, effects of recent revisions to the geomagnetic reversal time scale on estimates of current plate motions, geophysical research letters, v. 21, n. 20 pp.
* demets, c., gordon, r., argus, d., stein, s., 1994, effects of recent revisions to the geomagnetic reversal time scale on estimates of current plate motions, geophysical research letters, v. 21, n. 20 pp.
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