Realization of freestanding InP membranes on Si by low-temperature wafer bonding and stress analysis using micro-Raman spectroscopy

2006 ◽  
Vol 88 (22) ◽  
pp. 221901 ◽  
Author(s):  
J. Arokiaraj ◽  
S. Tripathy ◽  
S. Vicknesh ◽  
A. Ramam
Keyword(s):  
Raman Spectroscopy ◽  
Low Temperature ◽  
Stress Analysis ◽  
Wafer Bonding ◽  
Micro Raman Spectroscopy

Stress analysis of Si chip sidewalls using micro-Raman spectroscopy

2020 ◽  
Author(s):  
Martin De Biasio ◽  
Martin Kraft ◽  
Richard Ong ◽  
Christian Seifert ◽  
Manfred Ossiander ◽  
...  
Keyword(s):  
Raman Spectroscopy ◽  
Stress Analysis ◽  
Micro Raman Spectroscopy

scholarly journals Meridianiite detected in ice

2009 ◽  
Vol 55 (189) ◽  
pp. 117-122 ◽  
Author(s):  
F. Elif Genceli ◽  
Shinichirou Horikawa ◽  
Yoshinori Iizuka ◽  
Toshimitsu Sakurai ◽  
Takeo Hondoh ◽  
...  
Keyword(s):  
Raman Spectroscopy ◽  
Low Temperature ◽  
Sea Ice ◽  
Magnesium Sulfate ◽  
Raman Spectra ◽  
Sulfate Salt ◽  
Micro Raman Spectroscopy ◽  
Naturally Occurring ◽  
Formation History ◽  
History Of

AbstractInclusions affect the behavior of ice, and their characteristics help us understand the formation history of the ice. Recently, a low-temperature magnesium sulfate salt was discovered. This paper describes this naturally occurring MgSO4·11H2O mineral, meridianiite, derived from salt inclusions in sea ice of Lake Saroma, Japan and in Antarctic continental core ice. Its occurrence is confirmed by using micro-Raman spectroscopy to compare Raman spectra of synthetic MgSO4·11H2O with those of the inclusions.

scholarly journals Composition and stress analysis in Si structures using micro-raman spectroscopy

Scanning ◽  
2006 ◽  
Vol 26 (5) ◽  
pp. 235-239 ◽  
Author(s):  
J. McCarthy ◽  
T. S. Perova ◽  
R. A. Moore ◽  
S. Bhattacharya ◽  
H. Gamble ◽  
...  
Keyword(s):  
Raman Spectroscopy ◽  
Stress Analysis ◽  
Micro Raman Spectroscopy

T0302-2-2 Local stress analysis of single-crystalline resonator using micro Raman spectroscopy

2010 ◽  
Vol 2010.8 (0) ◽  
pp. 255-256
Author(s):  
Akira TANIYAMA ◽  
Yoshikazu HIRAI ◽  
Koji SUGANO ◽  
Osamu TABATA ◽  
Tsuyoshi IKEHARA ◽  
...  
Keyword(s):  
Raman Spectroscopy ◽  
Stress Analysis ◽  
Local Stress ◽  
Single Crystalline ◽  
Micro Raman Spectroscopy

Stress analysis in melt processed RBa2Cu3O7 (R=Y, Nd) by micro-Raman spectroscopy

1998 ◽  
Vol 6 (2-5) ◽  
pp. 185-192
Author(s):  
R Provoost ◽  
K Rosseel ◽  
D Dierickx ◽  
R.E Silverans ◽  
V.V Moshchalkov ◽  
...  
Keyword(s):  
Raman Spectroscopy ◽  
Stress Analysis ◽  
Micro Raman Spectroscopy

scholarly journals Evaluation of Deformation Temperatures in Carbonate Mylonites at Low Temperature Thrust-Tectonic Settings via Micro-Raman Spectroscopy

Minerals ◽  
2020 ◽  
Vol 10 (12) ◽  
pp. 1068
Author(s):  
Alessandro Croce ◽  
Enrico Pigazzi ◽  
Patrizia Fumagalli ◽  
Caterina Rinaudo ◽  
Michele Zucali
Keyword(s):  
Raman Spectroscopy ◽  
Low Temperature ◽  
Carbonate Rocks ◽  
Carbonaceous Material ◽  
Fold Belt ◽  
Micro Raman Spectroscopy ◽  
Axial Part ◽  
Laser Sources ◽  
Tectonic Settings ◽  
532 Nm

Carbonaceous materials (CMs) have been widely used to assess temperatures in sedimentary and metamorphic carbonate rocks. The use of Raman spectroscopy of carbonaceous material (RSCM) is largely devoted to the study of deformed rocks hosted in thrust-tectonic settings. Raman spectroscopy of carbonaceous material successfully allows the study of carbonate rocks at a temperature as high as 650 °C. In this study, a set of carbonate-mylonite rocks (Italian Alps) were investigated using micro-Raman spectroscopy, in order to infer the deformation conditions associated with the Alpine thrusts, expected to occur at T < 350 °C. Micro-Raman spectra were collected using two sources: green (532 nm) and red (632.8 nm) lasers. Several deconvolution procedures and parameters were tested to optimize the collected spectrum morphologies for the laser sources, also in accordance with the low temperature expected. The obtained temperatures highlight two clusters: one at 340–350 °C for the samples collected in the axial part of the Alpine chain, and the other at 200–240 °C for those collected in the external thrust-and-fold belt. These results agree with the independent geological and petrological constraints. Consistent results were obtained using 532 and 632.8 nm laser sources when the appropriate deconvolution approach was used.

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