Earth's heat

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Earth's heat

机译：地球的热量

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Our understanding of the thermal structure of oceanic lithosphere is based upon observations of water-loaded subsidence and plate age. These observations are predominantly from areas with sparse sedimentary cover, which are unperturbed by crustal thickening and by regional epeirogeny. Few such measurements are available from old oceanic lithosphere where sediment thickness is large.

机译：我们对海洋岩石圈热结构的理解是基于对水负沉和板块年龄的观察。这些观测资料主要来自沉积物稀少的地区，这些地区不受地壳增厚和区域成岩作用的干扰。沉积物厚度大的古老海洋岩石圈几乎没有这种测量方法。

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《Oceanographic Literature Review》 |2010年第1期|79-80|共2页
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Earth's heat

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