Sentence examples for magma was found from inspiring English sources

For deeper high-temperature wells like the IDDP-2 and K-36 wells in Iceland, several wells at Los Humeros, Mexico, the Prati 32 well at The Geysers, IDD-14 at Salton Sea, KS-2 in Hawaii, USA, and Sasso 22 and San Vito 1 in Italy, no molten magma was found.

Geochemically the charnockites of this region has been characterized as Tonalite and the charnockitic magma is found to have originated from a middle crustal region due to crustal recycling and is calc alkaline in nature.

As expected, the Magmas was found associated with membrane pellet fraction like Tim44, Tim23, Tim17, yPam18 and DnaJC19, whereas soluble matrix protein Mge1 (in yeast) and hTid1 (in human) were released into the supernatant in both high and low salt conditions (Fig.  2D and E).

Our results clearly indicate the cytoprotective role of Magmas that was found to protect all the major biomolecules, lipids, DNA and protein, from oxidative damage.

The function of Magmas as a ROS sensor was found to be independent of its role in protein import.

Contrastingly, in cells expressing Magmas mutants, the damage to DNA was found to be comparatively higher even in the absence of oxidative stress.

Originally, Magmas was identified as a protein involved in granulocyte-macrophage colony-stimulating factor (GM-CSF) signaling and was found to localize in mitochondria.

Wells encountering molten magma have been found to have a reasonable permeability in reservoir layers above the magma.

Hydrothermal fluid and a magma body were found to be present at depths of 3 10 km and greater than approximately 10 km, respectively, under Hakone volcano using seismic tomography (Yukutake et al. 2015).

Such rhyolitic magma can be found at the western part of the Anahim Volcanic Belt, which contrasts the more basaltic material in the Nazko Cone area.

To further support the CoIP analysis, all Magmas mutants were found defective in inhibiting DnaJC19 ATPase stimulation (Fig.  9C).