Q. Zhang et al., GEOCHEMICAL CHARACTERISTICS AND GENESIS OF DACHADABAN OPHIOLITE IN NORTH QILIAN AREA, SCIENCE IN CHINA SERIES D-EARTH SCIENCES, 41(3), 1998, pp. 277-281
There are three groups of pillow volcanics in the Dachadaban ophiolite
. Group 1 is typical boninite, enriched in Si, Mg and depleted.in Ti,
HREE and.HFSE; group 2 is the evolved boninite, slightly higher abunda
nce of Ti, HREE, HFSE and.large variation of Mg' due to fractional cry
stallization; and group 3 is tholeiite with MORE : character. The exis
tence of MORB and boninite indicates;hat the Dachadaban ophiolite was
probably formed in island-arc and back-arc environments.