نتایج جستجو برای: burial metamorphism

تعداد نتایج: 7218  

ایزدیار, جواد, ترکیان, اشرف, رضوانی مکبر, زهرا, سپاهی, علی اصغر,

Metamorphic area, which is a subject of this study, is located in S-Qorveh (Zarineh region), northwest of the Sanadaj-Sirjan zone. According to the recent dating, the S-Qorveh plutonic body consists of a complex of granitoids, granodiorites, quartz monzonites, and gabbros, have intruded into the host metamorphic rocks, about 149-152 Ma and have generated contact metamorphism. Intrusions of vari...

زینلی, ابراهیم, سلطانی, افشین, سلطانی, الیاس, قادری فر, فرشید, گالشی, سراله,

The aim of this study was to investigate and to quantify the effect of burial depth on seedling emergence of volunteer canola and wild mustard. Seeds were buried in 12 different depths (1, 2, 3, 4, 5, 6, 8, 10, 12, 15, 20, 30 cm) in 4 replications and seedling emergence was measured daily. Results indicated that emergence percentage of volunteer canola was around 98 % from 1 to 2.9 cm of burial...

Journal: :Science 2004
Pierre Cartigny Ingrid Chinn K S Viljoen Derek Robinson

Microdiamonds from the Akluilâk minette dykes (Nunavut, Canada) are similar to diamonds formed in subducted metamorphic rocks. High concentrations of unaggregated nitrogen and positive delta(15)N suggest that the microdiamonds formed within rocks subducted to ultrahigh pressures before being sampled by the minette magma 1.8 billion years ago. This ultrahigh pressure metamorphism in North Americ...

Journal: :Geological Magazine 1891

2011
Colin K. Grissom Chris H. Harmston Mary Beth Scholand Tim J. Bywater

Core body temperature cooling during avalanche burial results in hypothermia, and further core temperature cooling during extrication and evacuation of an avalanche burial victim may result in more severe hypothermia. We performed two studies measuring the rate of core body temperature cooling during snow burial and after extrication from snow burial. Subjects were completely buried in a large ...

Journal: :Geological Magazine 1895

Journal: :Journal of Geography (Chigaku Zasshi) 1988

Journal: :Geological Magazine 1891

Journal: :Geological Magazine 1890

,

The study area is located about 110 kilometers southeast of Mashhad and approximately 40 kilometers southeast of Fariman. The area is considered to be a part of the central Iran zone. It includes metamorphic rocks with different protoliths consisting of pelitic, carbonate and quartz - feldspathic rocks. The metamorphism in the study area is considered to be a contact regional metamorphism with ...

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