نتایج جستجو برای: serpentine soils

تعداد نتایج: 50431  

2000
M. Lampton

We demonstrate a multilayer circuit board that has two orthogonal serpentine delay lines on different layers to read out event positions from a microchannel plate ~MCP!. The top serpentine is directly bombarded by the MCP. The orthogonal buried serpentine receives its charge through thousands of vias that connect to the top surface. Event X and Y positions are decoded with a timing circuit for ...

یزدانی, مریم, آهنگری, معصومه , جهانگیری, احمد ,

Olivine is one of the major crystals in ultrabasic rocks of Piranshahr Ophiolitic Complex. This mineral occurs as anhedral with cracks and fractures. Commonly, olivine is altered to serpentine along the fractures and rims. In some cases, serpentine crosscut the olivine. According to BSE images and mineral chemistry studies of olivine, the secondary iron- rich olivines occur at the rim of primar...

2010
Young Ha Jeong Jong Yeon Kim Youn Moo Koo Jong Wook Choi Kum Whang Chul Hu Sung Min Cho

Giant serpentine aneurysms are uncommon types of aneurysmal disease and have angiographically authentic features. We report a case of a 44-year-old male with headache and seizure. He presented a giant serpentine aneurysm arising from the middle cerebral artery (MCA). It was a large intracranial aneurysm thrombosed as a mass-like lesion while it maintained its outflow drainage into the distal MC...

2009

Biological snakes’ diverse locomotion modes and physiology make them supremely adapted for environment. When their unique movements are broadly classified, the following four gliding modes exist: 1) Serpentine locomotion; 2) Rectilinear locomotion; 3) Concertina locomotion; 4) Side winding locomotion. However, the serpentine locomotion is the movement seen typically in almost all kinds of snake...

2010
B. L. Ehlmann J. F. Mustard S. L. Murchie

[1] Serpentine, recently discovered on Mars using Mars Reconnaissance Orbiter data, is uncommon but found in three geologic settings: (1) in mélange terrains at the Claritas Rise and the Nili Fossae, (2) associated with a few southern highlands impact craters, and (3) associated with a regional olivine‐rich stratigraphic unit near the Isidis basin. Any presently active serpentinization processe...

2008
Cin-Ty Aeolus Lee Peter Luffi Tobias Höink Zheng-Xue A. Li Adrian Lenardic

Cratons form the cores of continents and were formed within a narrow window of time (2.5–3.2 Gy ago), the majority having remained stable ever since. Petrologic evidence suggests that the thick mantle roots underlying cratons were built by underthrusting of oceanic and arc lithosphere, but paradoxically this requires that the building blocks of cratons are weak even though cratons must have bee...

Journal: :American journal of botany 2001
A E Pepper L E Norwood

Intra- and interspecific phylogenetic relationships of the rare serpentine endemic taxon Caulanthus amplexicaulus var. barbarae and related taxa in the "Streptanthoid Complex" of genera (Streptanthus, Caulanthus, Guillenia) were examined using nuclear ribosomal internal transcribed spacer (ITS) and chloroplast trnL intron sequences. Phylogenetic hypotheses generated from 81 variable ITS nucleot...

2017
Timothy A. Goudge James M. Russell John F. Mustard James W. Head Satria Bijaksana

Sediment deposited within lake basins can preserve detailed records of past environmental conditions on planetary surfaces, including both Earth and Mars. Establishing how to best characterize these paleoclimate records is thus critical for understanding the evolution of past planetary climates. Here, we present an ~40 k.y. lake sediment record from Lake Towuti, Indonesia, developed using visib...

2016
M. R. LEE

Forsterite and clinoenstatite in type IAB chondrules from the Murchison CM carbonaceous chondrite have been partially serpentinized, and the mechanisms of their alteration reveal crystallographic and microstructural controls on the reaction of silicate minerals with parent body aqueous solutions. Grains of forsterite were altered in two stages. Narrow veinlets of Fe-rich serpentine formed first...

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