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Zircon U-Pb Geochronology and Hf Isotopic Constraints on Petrogenesis of Plagiogranite from the Cuomuqu Ophiolite, Bangong Lake Area, North Tibet
Field observation, geochemical signatures and zircon Hf isotope data indicate that Cuomuqu ophiolite in the Bangonghu area was formed in a back-arc basin (BAB) above a supra-subduction zone (SSZ).Expand
Tectonic Evolution of the Meso-Tethys in the Western Segment of Bangonghu-Nujiang Suture Zone: Insights from Geochemistry and Geochronology of the Lagkor Tso Ophiolite
The subduction of the Bangonghu-Nujiang Meso-Tethys and the collision between the Lhasa and Qiangtang blocks were important events in the growth of the Tibetan crust. However, the timing of collisionExpand
Cenozoic Tectonic Evolution Sequence in Northern South China Sea and Its Oil/Gas Singificance
Based on the basic theory of tectonic geology,this study analyzed major tectonic events and tectonic evolution sequence in the Cenozoic through comprehensive investigation of geological effects suchExpand
The effect of the photoperiod on the growth and development of Semiothisa cinereari.
Exposure to 8-14 h of light extended the pupal overwintering period but this decreased when pupae were exposed to 14-16 h ofLight and the duration of pupae shortest, under an L:D ratio of 0:24. Expand