Game Analysis in Men’s University Basketball Game : For Hokushinetsu University of Basketball League in Division 1

バスケットボールについての研究では、選手個人やチームの技能を向上させることを目的としてさまざまなゲーム分析が実践されてきた。しかし、これまで行われてきた分析対象はトップカテゴリーが多く、地方の大学を対象としたものはほとんどない。そこで、本研究では北信越大学バスケットボール連盟男子1部リーグを対象に、試合中のどの要素が勝敗に影響を及ぼすか検討することを目的にゲーム分析を実施した。分析対象は第48回笹本杯争奪北信越大学バスケット ボール春季リーグ戦男子1 部リーグ全10試合とし、各試 合の勝ったチームの結果を勝ちチーム群、負けたチーム の結果を負けチーム群に分けて2群の比較を行った。分 析項目は、総得点、3ポイントシュート、2ポイント シュート、フリースロー、リバウンド、ターンオーバー、 攻撃回数とした。分析結果は総得点、3ポイントシュート（試投数、成功数、成功率）、2ポイントシュート（成功数）、攻撃効率に有意な差がみられた。その他の項目には有意な差は見られず、北信越大学リーグの特徴として、3ポイントシュートが勝敗に大きな影響を及ぼし、アウトサイドで 攻撃を展開していることが示唆された。Objectives ： The purpose of this research is to analyze the basketball game for Hokushinetsu University of Basketball League, and to clarify the tendency of the games.Methods ： Ten games of Men’s Hokushinetsu University of Basketball League in Division 1 were registered for this study. The analysis item was assumed to be total points, two points shot, three points shot, free throw, rebound, turnover, and possession.Results : The group of winner team indicated a value that was higher than the defeat team by total points, three points shot, two points shot and total points/possession.Whereas, two points shot, free throw, rebound, turnover didn’t have the influence.Conclusion : This result may indicate that the exterior shot is effectively used as a tendency to the win team in Hokushinetsu University of Basketball League.This has important implications for working out the tactic, and must be need further study

Indian Monsoonal Variations During the Past 80 Kyr Recorded in NGHP-02 Hole 19B, Western Bay of Bengal: Implications From Chemical and Mineral Properties

金沢大学理工研究域地球社会基盤学系Detailed reconstruction of Indian summer monsoons is necessary to better understand the late Quaternary climate history of the Bay of Bengal and Indian peninsula. We established a chronostratigraphy for a sediment core from Hole 19B in the western Bay of Bengal, extending to approximately 80 kyr BP and examined major and trace element compositions and clay mineral components of the sediments. Higher δ 18 O values, lower TiO 2 contents, and weaker weathering in the sediment source area during marine isotope stages (MIS) 2 and 4 compared to MIS 1, 3, and 5 are explained by increased Indian summer monsoonal precipitation and river discharge around the western Bay of Bengal. Clay mineral and chemical components indicate a felsic sediment source, suggesting the Precambrian gneissic complex of the eastern Indian peninsula as the dominant sediment source at this site since 80 kyr. Trace element ratios (Cr/Th, Th/Sc, Th/Co, La/Cr, and Eu/Eu*) indicate increased sediment contributions from mafic rocks during MIS 2 and 4. We interpret these results as reflecting the changing influences of the eastern and western branches of the Indian summer monsoon and a greater decrease in rainfall in the eastern and northeastern parts of the Indian peninsula than in the western part during MIS 2 and 4. © 2018. American Geophysical Union. All Rights Reserved

Magnetic Moment of Cu-Modified Ni2MnGa Magnetic Shape Memory Alloys

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