Diamond formation

Doeppner, T.; Falcone, R.W.; Glenzer, S.H.; Roth, M. Nanosecond formation of diamond and lonsdaleite by shock compression of graphite. Nature Communications

Association of Local Agency Formation Commissions. [August 25, 2014]. （原始内容 (Word)存档于November 3, 2014）.  Council Members. City of Diamond Bar. [December 16, 2014]

mystery of planet formation. CNN.com. April 5, 2006 [2006-04-05]. （原始内容存档于2006-04-08）.  Max Planck Institute, "A Planet made of Diamond" 互联网档案馆的存檔，存档日期2011-09-14

makes it more durable than a monocrystalline diamond. It is the same hardness as other types of diamond, but it is much tougher. Its polycrystalline texture

說中的妖精為名；種名在拉丁文意為「有長冠的」。 長冠妖精翼龍的正模標本（編號MN 6591-V）發現於巴西東北部的桑塔那組（Santana Formation），地質年代為白堊紀早期。正模標本包含口鼻部、一些部分翼部骨頭。妖精翼龍的成年個體，大型頭冠從口鼻部前段延伸到頭顱骨後方。根據之後發現的更多