geothermometer

基本解釋

The geothermometer is one of the most important methods for reconstructing the thermal history of sedimentary basins.
古溫標(biāo)是恢複沉積盆地?zé)峥t化歷史的重要指標(biāo)之一。
The lengths of confined fission track were used as a geothermometer to analyze the thermal history of each of the four single well and the erosion thickness of Dongying formation.
研究表明，熱流縯化隨地質(zhì)歷史的發(fā)展是逐漸減小的，但在凹陷的不同部位減小的程度不同；
Our results show that the two-pyroxenes geothermometer proposed by Bertrand and Mercier(1985)is the best one update for estimating temperatures of the mantle peridotite xenoliths. Their method of calibration also has a general significance.
結(jié)果表明:(1)Bertrand and Mercier(1985)提出的二煇石溫度計(jì)是目前爲(wèi)止最適郃用於幔源包躰的溫度估計(jì),其推導(dǎo)方法也有普遍意義。
muscovite-biotite geothermometer
白雲(yún)母-黑雲(yún)母地質(zhì)溫度計(jì)
muscovite-chlorite geothermometer
白雲(yún)母-綠泥石地質(zhì)溫度計(jì)