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Items: 4

1.

Metastable silica high pressure polymorphs as structural proxies of deep Earth silicate melts.

Bykova E, Bykov M, Černok A, Tidholm J, Simak SI, Hellman O, Belov MP, Abrikosov IA, Liermann HP, Hanfland M, Prakapenka VB, Prescher C, Dubrovinskaia N, Dubrovinsky L.

Nat Commun. 2018 Nov 15;9(1):4789. doi: 10.1038/s41467-018-07265-z.

2.

High pressure minerals in the Château-Renard (L6) ordinary chondrite: implications for collisions on its parent body.

Baziotis I, Asimow PD, Hu J, Ferrière L, Ma C, Cernok A, Anand M, Topa D.

Sci Rep. 2018 Jun 29;8(1):9851. doi: 10.1038/s41598-018-28191-6.

3.

Compressional pathways of α-cristobalite, structure of cristobalite X-I, and towards the understanding of seifertite formation.

Černok A, Marquardt K, Caracas R, Bykova E, Habler G, Liermann HP, Hanfland M, Mezouar M, Bobocioiu E, Dubrovinsky L.

Nat Commun. 2017 Jun 7;8:15647. doi: 10.1038/ncomms15647.

4.

Planetary science. Shock compression of stishovite and melting of silica at planetary interior conditions.

Millot M, Dubrovinskaia N, Černok A, Blaha S, Dubrovinsky L, Braun DG, Celliers PM, Collins GW, Eggert JH, Jeanloz R.

Science. 2015 Jan 23;347(6220):418-20. doi: 10.1126/science.1261507.

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