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一个钻石三部曲:超级地幔柱、超级大陆和超新星。

A diamond trilogy: superplumes, supercontinents, and supernovae.

作者信息

Haggerty SE

机构信息

Department of Geosciences, University of Massachusetts, Amherst, MA 01003, USA.

出版信息

Science. 1999 Aug 6;285(5429):851-60. doi: 10.1126/science.285.5429.851.

Abstract

Diamond is a remarkable mineral and has been long recognized for its unusual physical and chemical properties: robust and widespread in industry, yet regally adorned. This diversity is even greater than formally appreciated because diamond is recognized as an extraordinary recorder of astrophysical and geodynamic events that extend from the far reaches of space to Earth's deep interior. Many diamonds are natural antiques that formed in presolar supernovae by carbon vapor deposition, in asteroidal impacts and meteorite craters by shock metamorphism, and in Earth's mantle 1 to 2 billion years after planetary accretion from fluids and melts. The carbon in diamond is primordial, but there are unexplained isotopic fractionations and uncertainties in heterogeneity.

摘要

钻石是一种非凡的矿物,长期以来因其独特的物理和化学性质而闻名:在工业中用途广泛且举足轻重,同时又备受尊崇。这种多样性甚至比人们正式认识到的还要大,因为钻石被认为是天体物理和地球动力学事件的非凡记录者,这些事件从遥远的太空延伸到地球的深部内部。许多钻石是天然古董,它们在太阳系前超新星中通过碳气相沉积形成,在小行星撞击和陨石坑中通过冲击变质作用形成,以及在行星吸积后10亿到20亿年从地球地幔中的流体和熔体中形成。钻石中的碳是原始的,但存在无法解释的同位素分馏和不均匀性方面的不确定性。

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