start-ver=1.4
cd-journal=joma
no-vol=45
cd-vols=
no-issue=
article-no=
start-page=
end-page=
dt-received=
dt-revised=
dt-accepted=
dt-pub-year=1976
dt-pub=19760325
dt-online=
en-article=
kn-article=
en-subject=
kn-subject=
en-title=
kn-title=裏表紙
en-subtitle=
kn-subtitle=
en-abstract=
kn-abstract=
en-copyright=
kn-copyright=

en-aut-name=Institute for Thermal Spring Research, Okayama University
en-aut-sei=Institute for Thermal Spring Research, Okayama University
en-aut-mei=
kn-aut-name=岡山大学温泉研究所
kn-aut-sei=岡山大学温泉研究所
kn-aut-mei=
aut-affil-num=1
ORCID=

affil-num=1
en-affil=
kn-affil=
END

start-ver=1.4
cd-journal=joma
no-vol=45
cd-vols=
no-issue=
article-no=
start-page=
end-page=
dt-received=
dt-revised=
dt-accepted=
dt-pub-year=1976
dt-pub=19760325
dt-online=
en-article=
kn-article=
en-subject=
kn-subject=
en-title=
kn-title=奥付
en-subtitle=
kn-subtitle=
en-abstract=
kn-abstract=
en-copyright=
kn-copyright=

en-aut-name=Institute for Thermal Spring Research, Okayama University
en-aut-sei=Institute for Thermal Spring Research, Okayama University
en-aut-mei=
kn-aut-name=岡山大学温泉研究所
kn-aut-sei=岡山大学温泉研究所
kn-aut-mei=
aut-affil-num=1
ORCID=

affil-num=1
en-affil=
kn-affil=
END

start-ver=1.4
cd-journal=joma
no-vol=45
cd-vols=
no-issue=
article-no=
start-page=69
end-page=73
dt-received=
dt-revised=
dt-accepted=
dt-pub-year=1976
dt-pub=19760325
dt-online=
en-article=
kn-article=
en-subject=
kn-subject=
en-title=
kn-title=Oxygen Isotopic Data and Description of Rocks of the Yanai District in the Ryoke Belt, Japan
en-subtitle=
kn-subtitle=
en-abstract=
kn-abstract=
en-copyright=
kn-copyright=

en-aut-name=HonmaHiroji
en-aut-sei=Honma
en-aut-mei=Hiroji
kn-aut-name=本間弘次
kn-aut-sei=本間
kn-aut-mei=弘次
aut-affil-num=1
ORCID=

en-aut-name=SakaiHitoshi
en-aut-sei=Sakai
en-aut-mei=Hitoshi
kn-aut-name=酒井均
kn-aut-sei=酒井
kn-aut-mei=均
aut-affil-num=2
ORCID=

affil-num=1
en-affil=
kn-affil=Institute for Thermal Spring Research, Okayama University

affil-num=2
en-affil=
kn-affil=Institute for Thermal Spring Research, Okayama University
END

start-ver=1.4
cd-journal=joma
no-vol=45
cd-vols=
no-issue=
article-no=
start-page=47
end-page=67
dt-received=
dt-revised=
dt-accepted=
dt-pub-year=1976
dt-pub=19760325
dt-online=
en-article=
kn-article=
en-subject=
kn-subject=
en-title=On climatology in Misasa Spa (fourth report)
kn-title=三朝温泉地の気候について（第4報）
en-subtitle=
kn-subtitle=
en-abstract=Climatological data of the last three years (1972-1974) obtained at the observatory in the Branch Hospital of Okayama University Hospital at Misasa Spa, Tottori-ken, are presented.
kn-abstract=われわれは1956年1月以降,三朝温泉地の気候要素の観測を行ってきているが,今回は第4報として,1972年1月1日から1974年12月31日までの3カ年の気象観測の資料を報告することとした.
en-copyright=
kn-copyright=

en-aut-name=InoueTaeko
en-aut-sei=Inoue
en-aut-mei=Taeko
kn-aut-name=井上妙子
kn-aut-sei=井上
kn-aut-mei=妙子
aut-affil-num=1
ORCID=

en-aut-name=MorinagaHiroshi
en-aut-sei=Morinaga
en-aut-mei=Hiroshi
kn-aut-name=森永寛
kn-aut-sei=森永
kn-aut-mei=寛
aut-affil-num=2
ORCID=

affil-num=1
en-affil=
kn-affil=岡山大学医学部附属病院三朝分院内科

affil-num=2
en-affil=
kn-affil=岡山大学医学部附属病院三朝分院内科
END

start-ver=1.4
cd-journal=joma
no-vol=45
cd-vols=
no-issue=
article-no=
start-page=33
end-page=46
dt-received=
dt-revised=
dt-accepted=
dt-pub-year=1976
dt-pub=19760325
dt-online=
en-article=
kn-article=
en-subject=
kn-subject=
en-title=Genetic relationship between the Hiroshima and Ryoke granites as indicated by some geochemical evidence
kn-title=2･3の地球化学的特徴からみた広島花崗岩と領家花崗岩の成因的関係
en-subtitle=
kn-subtitle=
en-abstract=
kn-abstract=
en-copyright=
kn-copyright=

en-aut-name=HonmaHiroji
en-aut-sei=Honma
en-aut-mei=Hiroji
kn-aut-name=本間弘次
kn-aut-sei=本間
kn-aut-mei=弘次
aut-affil-num=1
ORCID=

affil-num=1
en-affil=
kn-affil=岡山大学温泉研究所地質学部門
END

start-ver=1.4
cd-journal=joma
no-vol=45
cd-vols=
no-issue=
article-no=
start-page=25
end-page=31
dt-received=
dt-revised=
dt-accepted=
dt-pub-year=1976
dt-pub=19760325
dt-online=
en-article=
kn-article=
en-subject=
kn-subject=
en-title=Studies on lithium in the field of balneology : Effects of lithium salts on analgesic activity of aminopyrine
kn-title=温泉医学領域におけるLithiumに関する研究--熱刺激に対するaminopyrineの鎮痛効果におよぼすLithium塩の影響
en-subtitle=
kn-subtitle=
en-abstract=
kn-abstract=The authors studied the effect of pretreatment with internal use of lithium salts on analgesic activity of aminopyrine by hot-plate test in mice. The male mice at 4 weeks of age weighting 17-19 g were divided into 7 groups. Earch group being composed of 9-10 mice was given oraBy 0.1 ml of LiCI-solution per 10 g of body weight for 35 days, LiCl was dissolved in 0.9% saline solution, in such concentrations that each group received 0 mg, 50 mg, 100mg, 200 mg and 400mg of LiCl for each kg of body weight of mouse, respectively, Control group received only 0.9% saline solution. On the 1st, 3rd, 7th, 14th, 21st, 28th and 35th days of this experiment, 0.1 ml of 1% solution of aminopyrine per 109 of body weight was injected intraperitoneaJly and then tested 30 minutes later. In the hot-plate test, a mouse is placed on a hot plate being adjusted with the thermostat at 55°±1℃, and the response is licking or lifting the hind feet or an outright attempt to escape from the plate, The increase in response time is used to quantify the analgesic effect of aminopyrine, The results were as follows : 1. The response time in groups receiving 0-50 mg of LiCl per kg of body weight had decreased on the 14 th day, but it tended to return to the initial level after the 21st day of experiment. 2. The response time in groups receiving 100-400 mg of LiCl per kg of body weight had also decreased on the 14 th day, and the degree of the decrease in response time was greater than that of the former and then remained faily constant at this level to the end of the observation period. These results would indicate that LiCl inhibits the analgesic activity of aminopyrine.
en-copyright=
kn-copyright=

en-aut-name=FurunoKatsushi
en-aut-sei=Furuno
en-aut-mei=Katsushi
kn-aut-name=古野勝志
kn-aut-sei=古野
kn-aut-mei=勝志
aut-affil-num=1
ORCID=

en-aut-name=MifuneMasaaki
en-aut-sei=Mifune
en-aut-mei=Masaaki
kn-aut-name=御船政明
kn-aut-sei=御船
kn-aut-mei=政明
aut-affil-num=2
ORCID=

affil-num=1
en-affil=
kn-affil=岡山大学温泉研究所温泉医学部門

affil-num=2
en-affil=
kn-affil=岡山大学温泉研究所温泉医学部門
END

start-ver=1.4
cd-journal=joma
no-vol=45
cd-vols=
no-issue=
article-no=
start-page=11
end-page=24
dt-received=
dt-revised=
dt-accepted=
dt-pub-year=1976
dt-pub=19760325
dt-online=
en-article=
kn-article=
en-subject=
kn-subject=
en-title=斜長石から生成したギブサイトの走査電顕観察―大山および三瓶山降下地積物中の粘土鉱物,その8―
kn-title=Scanning Electron Microscopic Study of Formation of Gibbsite From Plagioclase -The clay minerals in the Daisen loam and the Sambesan locm, Part 8-
en-subtitle=
kn-subtitle=
en-abstract=
kn-abstract=大山降下堆積物中の斜長石のギブサイト化過程を,偏光顕微鏡,X線,示差熱分析,走査型電顕,EPMAを用いて調べた. 斜長石は風化によって,カオリナイト,イライト,ハロイサイト,ギブサイト等を生成することが知られているが,今回,ギブサイト化した斜長石についてのみ検討をおこなった. EPMA分析によれば,一個の斜長石の表面に,Al, Si, Na, Caの多く存在する新鮮な斜長石の部分と,Na, Caをほとんど含まず,多量のAlと,ごく少量のSiを含んでいるギブサイトの部分とが分布し,その境界は, 明瞭であることがわかった（図版2）.それぞれの部分の分析値は第1表のとおりである. 走査型電顕による斜長石の微細形態観察から,下記のことが明らかになった. ①新鮮な斜長石の表面は,平滑かまたは離溶ラメラがみとめられる（図版3-1）. ②風化過程の初期に,水を合んだ非晶質の薄層が,斜長石の表層に生成する.この非晶質薄層の生成にさき立って,斜長石の表面の一部に, ロート状のくぼみが形成される場合がある（図版3-2,3）. ③この非晶質薄層に亀裂が生じる（図版4）.一方, ロート状のくぼみの上にも非晶質の薄層ができ,亀裂が生じる（図版8-1,2）. ④さらに風化が進むと,ラメラ, 亀裂およびロート状のくぼみを部分的に残しながら,-･部には,ギブサイトの結晶が生成する（図版5）. ⑤ギブサイトの結晶は,横1～3μm, 縦2～15μm,　厚さ0.5μm前後の平板状の形態,または,直径15-25μm,厚さ0.5～1μm の円盤上の形態をもつ（図版6）. ⑥ギブサイトの結晶は,平板状のものが数段重なり,集合体をなす場合もあり（図版7-1）,これは,ブラジルのミナス鉱山産のギブサイトの集合状態（図版7-2）とよく似ている. すなわち,斜長石の表面に,風化により,水を含んだ非晶質の薄層ができ,次に,その薄層に亀裂が生じ,イモゴライトの生成をともないながら,直接ギブサイトが結晶すると考えられる. 地名 Okachi 大河内　Hongu 本宮 Kurayoshi 倉吉 Daisen-Cho 大山町 Shuki 秋喜 Hiruzenbara 蒜山原
en-copyright=
kn-copyright=

en-aut-name=TazakiKazue
en-aut-sei=Tazaki
en-aut-mei=Kazue
kn-aut-name=田崎和江
kn-aut-sei=田崎
kn-aut-mei=和江
aut-affil-num=1
ORCID=

affil-num=1
en-affil=
kn-affil=岡山大学温泉研究所温泉地質学部門
END

start-ver=1.4
cd-journal=joma
no-vol=45
cd-vols=
no-issue=
article-no=
start-page=7
end-page=10
dt-received=
dt-revised=
dt-accepted=
dt-pub-year=1976
dt-pub=19760325
dt-online=
en-article=
kn-article=
en-subject=
kn-subject=
en-title=The effect of radioactive thermal bathing upon catecholamines of the whole brain of male mice
kn-title=マウスの脳内カテコールアミンに及ぼす温泉浴の影響について
en-subtitle=
kn-subtitle=
en-abstract=
kn-abstract=The author studied the changes of catecholamine levels of the whole brain of male mice weighing 15-20g before and after a single bathing for 20 minutes, 37±1℃ in temperature, in the radioactive hot spring in Misasa (Rn content : 74.83×10(-10)C/l), and compared the results obtained with those of the plain hot water bathing. The catecholamines (dopamine and noradrenaline) were measured by gaschromatographic method using electrone capture detector. It may be summarized as follows : 1. No significant change of dopamine and noradrenaline levels of the whole brain of mice was recognized before and after the plain hot water bathing used as a control. 2. Noradrenaline levels of the whole brain of mice had increased following the radioactive hot spring bath, and remained at same levels for 30 minutes after bathing. Dopamine levels had no change immediately after bathing, but had lowered at 30 minutes from the time of the bath. 3. Causes of these results are under investigation.
en-copyright=
kn-copyright=

en-aut-name=ItoKeiko
en-aut-sei=Ito
en-aut-mei=Keiko
kn-aut-name=伊東恵子
kn-aut-sei=伊東
kn-aut-mei=恵子
aut-affil-num=1
ORCID=

affil-num=1
en-affil=
kn-affil=岡山大学温泉研究所温泉医学部門
END

start-ver=1.4
cd-journal=joma
no-vol=45
cd-vols=
no-issue=
article-no=
start-page=1
end-page=6
dt-received=
dt-revised=
dt-accepted=
dt-pub-year=1976
dt-pub=19760325
dt-online=
en-article=
kn-article=
en-subject=
kn-subject=
en-title=Micromorphology of dendritic titanaugite
kn-title=樹枝状チタン輝石の微形態
en-subtitle=
kn-subtitle=
en-abstract=
kn-abstract=Dendritic titanaugite in ultrabasic picrite basalt from the Mineoka tectonic belt, Boso peninsula shows two contrastive morphology such as ; 1) ferny type and 2) skeletal type. Scanning electron microscopic observation reveals that there are three types of morphology as follows; 1) the cluster of needle crystals (Plate I-2, 3), 2) the pile of rail or fence like crystals (Plate II), 3) the stepped crystals (Plate III). The needle crystals have the cross section of distorted ellipsoid with 2 to 5μm in long diameter. The skeletal type morphology is ascribed to the cross section of the pile of rail or fence like crystals. The ferny type morphology comprises the clusters of needle and rail or fence like crystals.
en-copyright=
kn-copyright=

en-aut-name=TazakiKoichi
en-aut-sei=Tazaki
en-aut-mei=Koichi
kn-aut-name=田崎耕市
kn-aut-sei=田崎
kn-aut-mei=耕市
aut-affil-num=1
ORCID=

affil-num=1
en-affil=
kn-affil=岡山大学温泉研究所温泉地質学部門
END

start-ver=1.4
cd-journal=joma
no-vol=45
cd-vols=
no-issue=
article-no=
start-page=
end-page=
dt-received=
dt-revised=
dt-accepted=
dt-pub-year=1976
dt-pub=19760325
dt-online=
en-article=
kn-article=
en-subject=
kn-subject=
en-title=
kn-title=目次
en-subtitle=
kn-subtitle=
en-abstract=
kn-abstract=
en-copyright=
kn-copyright=

en-aut-name=Institute for Thermal Spring Research, Okayama University
en-aut-sei=Institute for Thermal Spring Research, Okayama University
en-aut-mei=
kn-aut-name=岡山大学温泉研究所
kn-aut-sei=岡山大学温泉研究所
kn-aut-mei=
aut-affil-num=1
ORCID=

affil-num=1
en-affil=
kn-affil=
END

start-ver=1.4
cd-journal=joma
no-vol=45
cd-vols=
no-issue=
article-no=
start-page=
end-page=
dt-received=
dt-revised=
dt-accepted=
dt-pub-year=1976
dt-pub=19760325
dt-online=
en-article=
kn-article=
en-subject=
kn-subject=
en-title=
kn-title=温研報執筆細則
en-subtitle=
kn-subtitle=
en-abstract=
kn-abstract=
en-copyright=
kn-copyright=

en-aut-name=Institute for Thermal Spring Research, Okayama University
en-aut-sei=Institute for Thermal Spring Research, Okayama University
en-aut-mei=
kn-aut-name=岡山大学温泉研究所
kn-aut-sei=岡山大学温泉研究所
kn-aut-mei=
aut-affil-num=1
ORCID=

affil-num=1
en-affil=
kn-affil=
END

start-ver=1.4
cd-journal=joma
no-vol=45
cd-vols=
no-issue=
article-no=
start-page=
end-page=
dt-received=
dt-revised=
dt-accepted=
dt-pub-year=1976
dt-pub=19760325
dt-online=
en-article=
kn-article=
en-subject=
kn-subject=
en-title=
kn-title=表紙
en-subtitle=
kn-subtitle=
en-abstract=
kn-abstract=
en-copyright=
kn-copyright=

en-aut-name=Institute for Thermal Spring Research, Okayama University
en-aut-sei=Institute for Thermal Spring Research, Okayama University
en-aut-mei=
kn-aut-name=岡山大学温泉研究所
kn-aut-sei=岡山大学温泉研究所
kn-aut-mei=
aut-affil-num=1
ORCID=

affil-num=1
en-affil=
kn-affil=
END