Study of diamonds from chromitites in the luobusa ophiolite, tibet

Acta Geologica Sinica (English Edition)

Volumn 75, Issue 3, 2001, Pages 409-

  Bai, W ^a   Yang, J ^a   Robinson, P ^a   Fang, Q ^a   Zhang, Z ^a   Yan, B ^a   Hu, X ^a  

^a INSTITUTE OF GEOLOGY   (China)

Author keywords

Diamond; Ophiolite; Tibet

Indexed keywords

CHROMITITE; DIAMOND; OPHIOLITE;

CHINA; TIBET;

EID: 0035161721     PISSN: 10009515     EISSN: 17556724     Source Type: Journal    
DOI: None     Document Type: Article

References (28)

1. Structure and evolution of the Himalaya-Tibet orogenic belt
2. An analyses about geological history of the Yarluzanbo plate suture zone and the Himalayas-Qinghai-Tibet plateau
3. There is no primary diamonds in the mantle peridotites of Luobusa and Donqiao
4. Tectonic implication of graphitised diamonds in the Ronda peridotite
5. Preliminary report on the serpentine and associated rock of Southern Quedec
6. The discovery of Alpine-type diamond-bearing ultrabasic intrution in Xizang (Tibet)
7. Graphitised diamonds from a peridotite massif in Morocco and implications for anomalous diamond occurrences
8. Graphite pseudomorphis after diamond
9. The genesis of podiform chromite deposits-A case study of the Luobosa Chromite deposit, Tibet
10. On the tectonic evolution of the Yarlu Zanbo (Tsangpo) suture zone and its adjacent areas