start-ver=1.4
cd-journal=joma
no-vol=43
cd-vols=
no-issue=
article-no=
start-page=
end-page=
dt-received=
dt-revised=
dt-accepted=
dt-pub-year=1974
dt-pub=19740325
dt-online=
en-article=
kn-article=
en-subject=
kn-subject=
en-title=
kn-title=裏表紙・英文目次
en-subtitle=
kn-subtitle=
en-abstract=
kn-abstract=
en-copyright=
kn-copyright=

en-aut-name=
en-aut-sei=
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=43
cd-vols=
no-issue=
article-no=
start-page=
end-page=
dt-received=
dt-revised=
dt-accepted=
dt-pub-year=1974
dt-pub=19740325
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=43
cd-vols=
no-issue=
article-no=
start-page=1
end-page=13
dt-received=
dt-revised=
dt-accepted=
dt-pub-year=1974
dt-pub=19740325
dt-online=
en-article=
kn-article=
en-subject=
kn-subject=
en-title=Phlogopites and coexisting pargasites in wehrlite from the northern Kanto mountains, central Japan
kn-title=北関東山地,単斜輝石かんらん岩の金雲母とパーガス閃石
en-subtitle=
kn-subtitle=
en-abstract=
kn-abstract=Coexisting interstitial phlogopites and pargasites in iron rich wehrlite from the northern Kanto mountains were studied. The textural relationｓ between those interstitial hydrous minerals and major constituent minerals, such as olivines and clinopyroxenes suggest the crystallization of the former from the intergranular residual liquids. The modal amounts of phlogopites in wehrlite are less than 1%, and that of pargasites range from 2 to 5%. Microprobe analyses have been carried for those hydrous minerals and the major constituent minerals. namely, olivine, clinopyroxene and idiomorphic zoned chromite. Olivines in wehrlite from the northern Kanto mountains have rather iron-rich nature and range from Foso to Fo(80) and those coexisting with the hydrous minerals are Fo(82.5) in average. Clinopyroxenes from mica bearing wehrlite contain about 2.5% Al(2)O(3). 17% MgO and 5.5% FeO. Tentative cation per cent of Ca, Mg and Fe are calculated as Ca(42.6) Mg(48.1) Fe(9.3) in average. The present probe analyses show high magnesian nature of the interstitial phlogopites. In addition, these phlogopites are conspicuous by their high TiO(2) content ranging from 4.6 to 5.2%. Mg/Mg + Fe versus Ti relation plotted in Fig. 4 revealed that the present phlogopite are similar to that of the alkaline pyroxenite nodules from the Lashaine volcano, northern Tanzania. Pargasites in mica bearing wehrlite are also rich in TiO(2) (3.0～4.7%), whereas pargasitic common hornblende from hornblendite or gabbro are rather low in TiO(2) (0.9～1.7%). Mg/Mg+Fe+Mn versus Ti relations of amphiboles illustrate that Ti contents increase with decrease of Mg/Mg+Fe +Mn. Two different increasing trend for Ti conten t are also noticed. Idiomorphic chromites show distinct compositional variation from core to rim. Total FeO increases about 16% at rim, whereas TiO(2), Al(2)O(3) and MgO decrease at the rim. Possible crystallization scheme of those hydrous minersls is proposed in Fig. 10, where the maximum stability limits of phlogopite and hornblende are shown with the curve for begining of melting of basalt. Separation of liquid fraction from cumulate phase with a small trapped intergranular liquid might occur at point A. The liquid fraction then might move upward through the course II. In cumulate phase, intergranular liquid might crystallize pargasitic amphibole by the reaction with olivine and clinopyroxene through the course I in Fig. 10. Intergranular liquid might decrease with production of amphiboles and K(2)O might concentrate in residual liquid. At final stage of crystallization, residual liquid rich in K(2)O might crystallize as phlogopite by the reactions with olivine. Decrease of Ti02 content at the nm of idiomorphic chromite might be related to the formations of Ti-rich hydrous minerals.
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=

en-aut-name=InomataMichiya
en-aut-sei=Inomata
en-aut-mei=Michiya
kn-aut-name=猪俣道也
kn-aut-sei=猪俣
kn-aut-mei=道也
aut-affil-num=2
ORCID=

affil-num=1
en-affil=
kn-affil=岡山大学温泉研究所

affil-num=2
en-affil=
kn-affil=東京教育大学理学部地質学鉱物学教室
END

start-ver=1.4
cd-journal=joma
no-vol=43
cd-vols=
no-issue=
article-no=
start-page=
end-page=
dt-received=
dt-revised=
dt-accepted=
dt-pub-year=1974
dt-pub=19740325
dt-online=
en-article=
kn-article=
en-subject=
kn-subject=
en-title=
kn-title=正誤表
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=43
cd-vols=
no-issue=
article-no=
start-page=
end-page=
dt-received=
dt-revised=
dt-accepted=
dt-pub-year=1974
dt-pub=19740325
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=43
cd-vols=
no-issue=
article-no=
start-page=
end-page=
dt-received=
dt-revised=
dt-accepted=
dt-pub-year=1974
dt-pub=19740325
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

start-ver=1.4
cd-journal=joma
no-vol=43
cd-vols=
no-issue=
article-no=
start-page=29
end-page=36
dt-received=
dt-revised=
dt-accepted=
dt-pub-year=1974
dt-pub=19740325
dt-online=
en-article=
kn-article=
en-subject=
kn-subject=
en-title=Continuous in-vIvo measurement of the brain tissue and the ischemic muscle gas tension using MEDSPECT, MS-8
kn-title=医用質量分析装置（MEDSPECT,MS-8型）を用いた脳および疎血肢の組織ガス分圧
en-subtitle=
kn-subtitle=
en-abstract=
kn-abstract=I MEDSPECT is a medical mass spectrometer for continuous in-vivo measurement of tissue, blood and respiratory gases. Interfacing catheter for tissue in measurement has Teflon membrane. The permeability and perfusion rate for various gases through its membrane varied with temperature. The temperature coefficient of Teflon catheter in the range of 15℃-40℃ is approximately constant with -2% of correction per degree for oxygen and carbon dioxide. Linear correlation was confirmed experimentally. II The brain tissue gas tensions were measured in ten dogs with intra-venous anesthesia at normothermia and deep hypothermia using perfusion cooling, including circulatory arrest for 30 minutes at 20°C of cerebral temperature. On average, the brain tissue P(O2) was 15mmHg in normothermia when the arterial P(O2) showed 95mmHg and the brain tissue P(CO2) was 49mmHg when the arterial PC02 showed 30mmHg. The brain tissue carbon dioxide tension gradually decreased by cooling and increased during circulatory arrest for 30 minutes; from 45mmHg to 72mmHg. The brain tissue oxygen tension increased during cooling from 15mmHg to 41mmHg and decreased in the circulatory arrest; from 41mmHg to 36mmHg. III The ischemic muscle gas tension was measured in a 22-year-old man, who was suffered from thromboangiitis obliterans bilaterally, and had the popliteal autovein bypass surgery 3 months ago. Control oxygen tensions in the both anterior tibial muscles showed about the same; 35mmHg and 36mmHg respectivelly, and the P(O2) of the non-operated side showed remarkable low level of 18mmHg as compared with the side of arterial reconstruction surgery after 5-minutes ankle exercise.
en-copyright=
kn-copyright=

en-aut-name=KawakamiShunji
en-aut-sei=Kawakami
en-aut-mei=Shunji
kn-aut-name=川上俊爾
kn-aut-sei=川上
kn-aut-mei=俊爾
aut-affil-num=1
ORCID=

en-aut-name=YamaneYoshihisa
en-aut-sei=Yamane
en-aut-mei=Yoshihisa
kn-aut-name=山根義久
kn-aut-sei=山根
kn-aut-mei=義久
aut-affil-num=2
ORCID=

en-aut-name=NoishikiYasuharu
en-aut-sei=Noishiki
en-aut-mei=Yasuharu
kn-aut-name=野一色泰晴
kn-aut-sei=野一色
kn-aut-mei=泰晴
aut-affil-num=3
ORCID=

en-aut-name=KomotoYoshiaki
en-aut-sei=Komoto
en-aut-mei=Yoshiaki
kn-aut-name=古元嘉昭
kn-aut-sei=古元
kn-aut-mei=嘉昭
aut-affil-num=4
ORCID=

en-aut-name=TeramotoShigeru
en-aut-sei=Teramoto
en-aut-mei=Shigeru
kn-aut-name=寺本滋
kn-aut-sei=寺本
kn-aut-mei=滋
aut-affil-num=5
ORCID=

en-aut-name=SenohYoshimasa
en-aut-sei=Senoh
en-aut-mei=Yoshimasa
kn-aut-name=妹尾嘉昌
kn-aut-sei=妹尾
kn-aut-mei=嘉昌
aut-affil-num=6
ORCID=

en-aut-name=KanekoKatsuya
en-aut-sei=Kaneko
en-aut-mei=Katsuya
kn-aut-name=金子克也
kn-aut-sei=金子
kn-aut-mei=克也
aut-affil-num=7
ORCID=

en-aut-name=SugimotoSeiki
en-aut-sei=Sugimoto
en-aut-mei=Seiki
kn-aut-name=杉本誠起
kn-aut-sei=杉本
kn-aut-mei=誠起
aut-affil-num=8
ORCID=

en-aut-name=TakahashiShunjiro
en-aut-sei=Takahashi
en-aut-mei=Shunjiro
kn-aut-name=高橋俊二郎
kn-aut-sei=高橋
kn-aut-mei=俊二郎
aut-affil-num=9
ORCID=

affil-num=1
en-affil=
kn-affil=岡山大学温泉研究所リハビリテーション医学部門

affil-num=2
en-affil=
kn-affil=岡山大学温泉研究所リハビリテーション医学部門

affil-num=3
en-affil=
kn-affil=岡山大学温泉研究所リハビリテーション医学部門

affil-num=4
en-affil=
kn-affil=岡山大学温泉研究所リハビリテーション医学部門

affil-num=5
en-affil=
kn-affil=岡山大学医学部第2外科学教室

affil-num=6
en-affil=
kn-affil=岡山大学医学部第2外科学教室

affil-num=7
en-affil=
kn-affil=岡山大学医学部第2外科学教室

affil-num=8
en-affil=
kn-affil=岡山大学医学部第2外科学教室

affil-num=9
en-affil=
kn-affil=岡山大学医学部第2外科学教室
END

start-ver=1.4
cd-journal=joma
no-vol=43
cd-vols=
no-issue=
article-no=
start-page=15
end-page=28
dt-received=
dt-revised=
dt-accepted=
dt-pub-year=1974
dt-pub=19740325
dt-online=
en-article=
kn-article=
en-subject=
kn-subject=
en-title=Hydrogen and oxygen isotopic ratios of thermal and mineral springs in Arima area
kn-title=有馬地域の温泉,鉱泉の水素と酸素の同位体比について
en-subtitle=
kn-subtitle=
en-abstract=
kn-abstract=Saline waters of thermal and mineral springs in Arima area, at Takarazuka, and in Ishibotoke area of Kawachinagano City indicate wide ranges of δD and δ(18)O values (Table 1). Excellent linearity exists between the δD and δ(18)O values (Fig. 1) and between the δ(18)O value and the chloride concentration (Fig. 2). These facts as well as the chemical evidence of the previous investigators strongly support the view that Arima springs are admixtures of a single deep brine and local ground water (TSURUMAKI, 1964). The deep brine may have the δ(18)O value of +8.0～+8.5‰, the δD value of -25～-30‰, and the chloride concentration of 1.20～1.25 eq/l, which were estimated from the water of the maximum salinity so far reported. Because the thermal and mineral springs in Arima area closely associate with the upper Cretaceous granitic rocks, and the estimated δ(18)O value of the deep brine is similar to a value of water in isotopic equilibrium with those granitic rocks at 500～600℃, the deep brine of Arima might have been the magmatic water of those granitic rocks. The mineral springs at Takarazuka and in Ishibotoke area also show the similar linearity among Cl(-), δ(18)O and δD to those in Arima area. Therefore it is assumed that the mineral springs at Takarazuka may be of the same origin as that in Arima area, and the mineral springs in Ishibotoke area might have been the fluid associated with Ryoke metamorphic rocks. Alternatively, the deep brine in Arima area may be isotopically and chemically similar to the saline formation waters in Illinois basin (GRAF et al., 1966). The high δD values and salinities of those formation waters were attributed to the isotopic and chemical fractionation during the passage of water through sediments. The deep brine in Arima area may be genetically similar to those saline formation waters. If such a saline water could have formed in Osaka basin, it is not surprising to find out the similar brines at Arima and Ishibotoke which are the northwestern and southeastern rims of the basin, respectively. At the present, it cannot be answered which of these two models is more probable. Further studies on other saline springs fluid inclusions of Cretaceous granitic rocks may be useful in order to solve this problem.
en-copyright=
kn-copyright=

en-aut-name=MatsubayaOsamu
en-aut-sei=Matsubaya
en-aut-mei=Osamu
kn-aut-name=松葉谷治
kn-aut-sei=松葉谷
kn-aut-mei=治
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=

en-aut-name=TsurumakiMichiji
en-aut-sei=Tsurumaki
en-aut-mei=Michiji
kn-aut-name=鶴巻道二
kn-aut-sei=鶴巻
kn-aut-mei=道二
aut-affil-num=3
ORCID=

affil-num=1
en-affil=
kn-affil=岡山大学温泉研究所化学部門

affil-num=2
en-affil=
kn-affil=岡山大学温泉研究所化学部門

affil-num=3
en-affil=
kn-affil=大阪市立大学理学部地学教室
END