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Year: 2008 ×Author: Feng Hong ×Clear All Filters
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Island Arc · 2008 · Vol. 17 · Issue 4 · Wiley
Pseudosections for two sediments and one basalt calculated in the system K 2 O–Na 2 O–CaO–MgO–FeO–Fe 2 O 3 –Al 2 O 3 –TiO 2 –SiO 2 –H 2 O for the P–T range 10 to 35 kbar, 300 to 900°C give useful insights into the amount of H 2 O released from oceanic crust in subduction zones. In cold subduction zones (20 kbar–300°C to 35 kbar–500°C) hydrous minerals storing 3 to 4 wt% H 2 O are still present in metasediments at depths of 120...
Environmental Microbiology · 2008 · Vol. 10 · Issue 7 · Wiley
Summary Resting spore formation of some aphid‐pathogenic Entomophthorales is important for the seasonal pattern of their prevalence and survival but this process is poorly understood. To explore the possible mechanism involved in the process, Pandora nouryi (obligate aphid pathogen) interacted with green peach aphid Myzus persicae on cabbage leaves under favourable conditions. Host nymphs showered with primary conidia of an is...
Island Arc · 2008 · Vol. 17 · Issue 2 · Wiley
The occurrence of the Pishikou mafic dike in the Qingdao region, China provides important constraints on the origin of Late Cretaceous (86–78 Ma) mafic magmatism on the eastern North China craton. The Pishikou mafic dike is distributed in the Cretaceous Laoshan granitoid body, Qingdao region and contains peridotitic and granulitic xenoliths, xenocrysts, and megacrysts. Rocks from the Pishikou mafic dike are basanites and have...