Made available in DSpace on 2014-10-09T12:50:39Z (GMT). No. of bitstreams: 0 / Made available in DSpace on 2014-10-09T13:58:59Z (GMT). No. of bitstreams: 1 00051.pdf: 1323615 bytes, checksum: 560d14914e0156e890a27864c7db81e2 (MD5) / Dissertacao (Mestrado) / IEA/D / Instituto de Fisica, Universidade de Sao Paulo - IF/USP

Made available in DSpace on 2014-10-09T12:50:39Z (GMT). No. of bitstreams: 0 / Made available in DSpace on 2014-10-09T13:58:59Z (GMT). No. of bitstreams: 1 00051.pdf: 1323615 bytes, checksum: 560d14914e0156e890a27864c7db81e2 (MD5) / Dissertacao (Mestrado) / IEA/D / Instituto de Fisica, Universidade de Sao Paulo - IF/USP

<p> This study describes the analysis of orientation of elongate quartz grains in massive turbidite sandstones from the Chetco Formation (Jurassic) of southwestern Oregon. Inferences on depositional fabric of this resedimented facies are made.</p> <p> Grain orientation in the plane parallel to bedding is generally not highly significant statistically, and current direction, supplied by imbrication, is not persistent vertically through the beds. However, a rotation pattern of current direction in each bed is detected.</p> <p> Variations in orientation distribution could represent variations in sediment concentration of the flow and in the rate of deposition.</p> / Thesis / Bachelor of Science (BSc)

This study describes the analysis of orientation of elongate quartz grains in turbidite greywackes of the Normanskill Formation, (Ord.) New York. No relationship is found between grain orientation and sole features of the beds. No relationship exists between grain orientations taken at different levels above the base of the beds. Maximum grain size and maximum elongation decrease upwards in the beds. The most elongate grains are those which most clearly show preferred orientation. / Thesis / Master of Science (MSc)

Made available in DSpace on 2014-10-09T12:45:37Z (GMT). No. of bitstreams: 0 / Made available in DSpace on 2014-10-09T14:07:15Z (GMT). No. of bitstreams: 1 07310.pdf: 8434532 bytes, checksum: 2fffac8743bcb0d1fd0d8045952b7835 (MD5) / Tese (Doutoramento) / IPEN/T / Instituto de Pesquisas Energeticas e Nucleares - IPEN/CNEN-SP

abstract: Microelectronic industry is continuously moving in a trend requiring smaller and smaller devices and reduced form factors with time, resulting in new challenges. Reduction in device and interconnect solder bump sizes has led to increased current density in these small solders. Higher level of electromigration occurring due to increased current density is of great concern affecting the reliability of the entire microelectronics systems. This paper reviews electromigration in Pb- free solders, focusing specifically on Sn0.7wt.% Cu solder joints. Effect of texture, grain orientation, and grain-boundary misorientation angle on electromigration and intermetallic compound (IMC) formation is studied through EBSD analysis performed on actual C4 bumps. / Dissertation/Thesis / M.S. English 2013

Made available in DSpace on 2014-10-09T12:45:37Z (GMT). No. of bitstreams: 0 / Made available in DSpace on 2014-10-09T14:07:15Z (GMT). No. of bitstreams: 1 07310.pdf: 8434532 bytes, checksum: 2fffac8743bcb0d1fd0d8045952b7835 (MD5) / Tese (Doutoramento) / IPEN/T / Instituto de Pesquisas Energeticas e Nucleares - IPEN/CNEN-SP

Missing page 10. / <p> Interbedded turbidite sandstones and shales of the Sonyea Group are exposed in the Finger Lakes Stone Quarry near Ithaca, New York. In 28% of the samples studied the orientation of the grains was not significantly different from a uniform distribution. These distributions included some that were bimodal and some obtained from a bed showing cross-stratification. In 60% of the samples the grain orientations could be considered parallel to the flute marks. As the top of the massive interval was approached the grain orientation became increasingly aligned with the flute marks. A difference of 14° was found between the vector means of the flute and tool marks. </p> <p> Radiographs made of rock slabs cut from the samples used in grain orientation determinations frequently failed to show internal structures even though these were visible in the samples. A radiograph of one sample (02-08) showed cross-bedding, not visible in the sample or slab. The absence of internal structures in a radiograph do not exclude their being present. </p> / Thesis / Bachelor of Science (BSc)

Made available in DSpace on 2014-10-09T12:43:57Z (GMT). No. of bitstreams: 0 / Made available in DSpace on 2014-10-09T14:08:19Z (GMT). No. of bitstreams: 1 06781.pdf: 5180316 bytes, checksum: 400f92bad2534a326e86a6f14c3ba5cb (MD5) / Dissertacao (Mestrado) / IPEN/D / Instituto de Pesquisas Energeticas e Nucleares - IPEN/CNEN-SP

Made available in DSpace on 2014-10-09T12:43:57Z (GMT). No. of bitstreams: 0 / Made available in DSpace on 2014-10-09T14:08:19Z (GMT). No. of bitstreams: 1 06781.pdf: 5180316 bytes, checksum: 400f92bad2534a326e86a6f14c3ba5cb (MD5) / Dissertacao (Mestrado) / IPEN/D / Instituto de Pesquisas Energeticas e Nucleares - IPEN/CNEN-SP