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CHIME ages o f monazi te from th e Shinshiro Tonal i te of the Ryoke b elt in the Mikawa area, Aichi P re f ec ture

by Taisei Morishita, Kazuhiro Suzuki , 1995
"... The Shinshiro Tonalite located on the north of the Median Tectonic Line in the Mikawa area is the oldest pluton among the post-tectonic intrusive in the eastern Ryoke belt. monazites recovered fron three samples of the leucocratic varieties of the Shinshiro Tonalite yiled CHIME ages of 86.0±4.7, 85. ..."
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.2±3.3 and 85.5±5.5 Ma. These ages, interpreted as the time of the emplacement, are some 1 5 Ma younger than the CHIME monazi te age s fo r the Ry ok e g ni es s, and slightly older than the CHIME monazite ages for the subsequent Mitsuhashi Granodiorite (ca. 84 Ma).

Clinical Chemistry 44:11 2256–2263 (1998) Molecular Diagnostics

by Genetics
"... Direct reverse transcription-PCR on oligo(dT)immobilized polypropylene microplates after capturing total mRNA from crude cell lysates Yohei Hamaguchi, 1,2 Yoshimasa Aso, 1 Hiroshi Shimada, 2 and Masato Mitsuhashi 1,3* To simplify gene expression analysis, oligo(dT)-immobilized polypropylene micropla ..."
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Direct reverse transcription-PCR on oligo(dT)immobilized polypropylene microplates after capturing total mRNA from crude cell lysates Yohei Hamaguchi, 1,2 Yoshimasa Aso, 1 Hiroshi Shimada, 2 and Masato Mitsuhashi 1,3* To simplify gene expression analysis, oligo(dT)-immobilized polypropylene
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