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STROPHOMENIDA ОРДОВИКА И СИЛУРА ЭСТОНИИ. III
Proceedings of the Academy of Sciences of the Estonian SSR. Geology Pub Date : 1900-01-01 DOI: 10.3176/geol.1981.2.04
A. Rõõmusoks
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引用次数: 0
О РАЦИОНАЛЬНОМ ОКОНТУРИВАНИИ БАЛАНСОВЫХ ЗАПАСОВ ФОСФОРИТНЫХ МЕСТОРОЖДЕНИЙ ЭСТОНСКОЙ ССР ПРИ ПОДЗЕМНОЙ ИХ РАЗРАБОТКЕ 爱沙尼亚ssr磷酸盐储量在地下开采时合理地减少了
Proceedings of the Academy of Sciences of the Estonian SSR. Geology Pub Date : 1900-01-01 DOI: 10.3176/geol.1983.1.03
R. Päsok
{"title":"О РАЦИОНАЛЬНОМ ОКОНТУРИВАНИИ БАЛАНСОВЫХ ЗАПАСОВ ФОСФОРИТНЫХ МЕСТОРОЖДЕНИЙ ЭСТОНСКОЙ ССР ПРИ ПОДЗЕМНОЙ ИХ РАЗРАБОТКЕ","authors":"R. Päsok","doi":"10.3176/geol.1983.1.03","DOIUrl":"https://doi.org/10.3176/geol.1983.1.03","url":null,"abstract":"","PeriodicalId":129290,"journal":{"name":"Proceedings of the Academy of Sciences of the Estonian SSR. Geology","volume":"7 1","pages":"0"},"PeriodicalIF":0.0,"publicationDate":"1900-01-01","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"131245784","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":0,"RegionCategory":"","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}
引用次数: 0
ЗНАЧЕНИЕ ПЕРЕОТЛОЖЕННОЙ ПЫЛЬЦЫ МЕЖЛЕДНИКОВЫХ ТЕРМОФИЛЬНЫХ ДРЕВЕСНЫХ ПОРОД В СТРАТИГРАФИИ 冰河间热风木质岩石重新沉积花粉值
Proceedings of the Academy of Sciences of the Estonian SSR. Geology Pub Date : 1900-01-01 DOI: 10.3176/geol.1982.2.05
E. Liivrand
{"title":"ЗНАЧЕНИЕ ПЕРЕОТЛОЖЕННОЙ ПЫЛЬЦЫ МЕЖЛЕДНИКОВЫХ ТЕРМОФИЛЬНЫХ ДРЕВЕСНЫХ ПОРОД В СТРАТИГРАФИИ","authors":"E. Liivrand","doi":"10.3176/geol.1982.2.05","DOIUrl":"https://doi.org/10.3176/geol.1982.2.05","url":null,"abstract":"","PeriodicalId":129290,"journal":{"name":"Proceedings of the Academy of Sciences of the Estonian SSR. Geology","volume":"254 1","pages":"0"},"PeriodicalIF":0.0,"publicationDate":"1900-01-01","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"121322205","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":0,"RegionCategory":"","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}
引用次数: 0
ТИПОМОРФНЫЕ ОСОБЕННОСТИ ЦИРКОНА ПОРОД КРИСТАЛЛИЧЕСКОГО ФУНДАМЕНТА ЭСТОНИИ 爱沙尼亚结晶基质锆的特殊性
Proceedings of the Academy of Sciences of the Estonian SSR. Geology Pub Date : 1900-01-01 DOI: 10.3176/geol.1986.1.01
M. Konsa
{"title":"ТИПОМОРФНЫЕ ОСОБЕННОСТИ ЦИРКОНА ПОРОД КРИСТАЛЛИЧЕСКОГО ФУНДАМЕНТА ЭСТОНИИ","authors":"M. Konsa","doi":"10.3176/geol.1986.1.01","DOIUrl":"https://doi.org/10.3176/geol.1986.1.01","url":null,"abstract":"","PeriodicalId":129290,"journal":{"name":"Proceedings of the Academy of Sciences of the Estonian SSR. Geology","volume":"90 1","pages":"0"},"PeriodicalIF":0.0,"publicationDate":"1900-01-01","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"121447127","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":0,"RegionCategory":"","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}
引用次数: 0
О ЛИТОЛОГИИ МОРЕН И ЛЕНТОЧНЫХ ГЛИН СО ДНА ВЯЙНАМЕРИ (ЗАПАДНАЯ ЭСТОНИЯ) 关于立陶宛学，莫雷诺和胶带粘土来自爱沙尼亚西部
Proceedings of the Academy of Sciences of the Estonian SSR. Geology Pub Date : 1900-01-01 DOI: 10.3176/geol.1980.2.03
J. Lutt
{"title":"О ЛИТОЛОГИИ МОРЕН И ЛЕНТОЧНЫХ ГЛИН СО ДНА ВЯЙНАМЕРИ (ЗАПАДНАЯ ЭСТОНИЯ)","authors":"J. Lutt","doi":"10.3176/geol.1980.2.03","DOIUrl":"https://doi.org/10.3176/geol.1980.2.03","url":null,"abstract":"","PeriodicalId":129290,"journal":{"name":"Proceedings of the Academy of Sciences of the Estonian SSR. Geology","volume":"25 1","pages":"0"},"PeriodicalIF":0.0,"publicationDate":"1900-01-01","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"116158781","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":0,"RegionCategory":"","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}
引用次数: 0
НЕКОТОРЫЕ МИНЕРАЛОГИЧЕСКИЕ АСПЕКТЫ ТЛ-ДАТИРО- ВАНИЯ И ПРОБЛЕМЫ ПОДГОТОВКИ ОБРАЗЦОВ
Proceedings of the Academy of Sciences of the Estonian SSR. Geology Pub Date : 1900-01-01 DOI: 10.3176/geol.1988.2.05
K. Vares
{"title":"НЕКОТОРЫЕ МИНЕРАЛОГИЧЕСКИЕ АСПЕКТЫ ТЛ-ДАТИРО- ВАНИЯ И ПРОБЛЕМЫ ПОДГОТОВКИ ОБРАЗЦОВ","authors":"K. Vares","doi":"10.3176/geol.1988.2.05","DOIUrl":"https://doi.org/10.3176/geol.1988.2.05","url":null,"abstract":"","PeriodicalId":129290,"journal":{"name":"Proceedings of the Academy of Sciences of the Estonian SSR. Geology","volume":"32 1","pages":"0"},"PeriodicalIF":0.0,"publicationDate":"1900-01-01","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"115300416","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":0,"RegionCategory":"","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}
引用次数: 0
О ГЕОЛОГИЧЕСКОЙ КОРРЕЛЯЦИИ ДРЕВНЕБЕРЕГОВЫХ ОБРАЗОВАНИЙ БАЛТИЙСКОГО МОРЯ В ЭСТОНИИ И ШВЕЦИИ 关于爱沙尼亚和瑞典波罗的海古海岸的地质关系
Proceedings of the Academy of Sciences of the Estonian SSR. Geology Pub Date : 1900-01-01 DOI: 10.3176/geol.1984.3/4.08
H. Kessel, A. Raukas
{"title":"О ГЕОЛОГИЧЕСКОЙ КОРРЕЛЯЦИИ ДРЕВНЕБЕРЕГОВЫХ ОБРАЗОВАНИЙ БАЛТИЙСКОГО МОРЯ В ЭСТОНИИ И ШВЕЦИИ","authors":"H. Kessel, A. Raukas","doi":"10.3176/geol.1984.3/4.08","DOIUrl":"https://doi.org/10.3176/geol.1984.3/4.08","url":null,"abstract":"","PeriodicalId":129290,"journal":{"name":"Proceedings of the Academy of Sciences of the Estonian SSR. Geology","volume":"142 1","pages":"0"},"PeriodicalIF":0.0,"publicationDate":"1900-01-01","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"116588926","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":0,"RegionCategory":"","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}
引用次数: 1
ПРИМЕНЕНИЕ МЕТОДА ПОЛИНОМИАЛЬНОЙ АППРОКСИМАЦИИ ДЛЯ ВЫДЕЛЕНИЯ ТЕНДЕНЦИЙ СКОРОСТИ РОСТА ТОРФЯНОЙ ЗАЛЕЖИ НА ПРИМЕРЕ БОЛОТА НИГУЛА 多项式近似法的应用，以尼古拉沼泽为例，突出泥炭生长速度的趋势
Proceedings of the Academy of Sciences of the Estonian SSR. Geology Pub Date : 1900-01-01 DOI: 10.3176/geol.1985.4.04
K. Orgla
{"title":"ПРИМЕНЕНИЕ МЕТОДА ПОЛИНОМИАЛЬНОЙ АППРОКСИМАЦИИ ДЛЯ ВЫДЕЛЕНИЯ ТЕНДЕНЦИЙ СКОРОСТИ РОСТА ТОРФЯНОЙ ЗАЛЕЖИ НА ПРИМЕРЕ БОЛОТА НИГУЛА","authors":"K. Orgla","doi":"10.3176/geol.1985.4.04","DOIUrl":"https://doi.org/10.3176/geol.1985.4.04","url":null,"abstract":"","PeriodicalId":129290,"journal":{"name":"Proceedings of the Academy of Sciences of the Estonian SSR. Geology","volume":"8 1","pages":"0"},"PeriodicalIF":0.0,"publicationDate":"1900-01-01","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"125280852","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":0,"RegionCategory":"","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}
引用次数: 0
НЕКОТОРЫЕ ЧЕРТЫ ФОРМИРОВАНИЯ ДОННЫХ ОСАДКОВ ВЯЙНАМЕРИ ПО ДАННЫМ ИХ ГРАНУЛОМЕТРИЧЕСКОГО СОСТАВА 根据它们的粒度组成，维米哈米里沉积物形成的一些特征
Proceedings of the Academy of Sciences of the Estonian SSR. Geology Pub Date : 1900-01-01 DOI: 10.3176/geol.1980.2.04
J. Lutt
{"title":"НЕКОТОРЫЕ ЧЕРТЫ ФОРМИРОВАНИЯ ДОННЫХ ОСАДКОВ ВЯЙНАМЕРИ ПО ДАННЫМ ИХ ГРАНУЛОМЕТРИЧЕСКОГО СОСТАВА","authors":"J. Lutt","doi":"10.3176/geol.1980.2.04","DOIUrl":"https://doi.org/10.3176/geol.1980.2.04","url":null,"abstract":"","PeriodicalId":129290,"journal":{"name":"Proceedings of the Academy of Sciences of the Estonian SSR. Geology","volume":"26 1","pages":"0"},"PeriodicalIF":0.0,"publicationDate":"1900-01-01","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"125243763","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":0,"RegionCategory":"","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}
引用次数: 0
THE TAUČIONYS FORMATION (HOLORHYNCHUS BEDS) IN THE ILJINSKOJE BORING (PSKOV DISTRICT) 伊尔金斯科耶钻孔(普斯科夫地区)tauČionys组(holorhynchus层)
Proceedings of the Academy of Sciences of the Estonian SSR. Geology Pub Date : 1900-01-01 DOI: 10.3176/geol.1989.2.10
L. Hints, T. Meidla, J. Nõlvak
{"title":"THE TAUČIONYS FORMATION (HOLORHYNCHUS BEDS) IN THE ILJINSKOJE BORING (PSKOV DISTRICT)","authors":"L. Hints, T. Meidla, J. Nõlvak","doi":"10.3176/geol.1989.2.10","DOIUrl":"https://doi.org/10.3176/geol.1989.2.10","url":null,"abstract":"","PeriodicalId":129290,"journal":{"name":"Proceedings of the Academy of Sciences of the Estonian SSR. Geology","volume":"1 1","pages":"0"},"PeriodicalIF":0.0,"publicationDate":"1900-01-01","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"130117529","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":0,"RegionCategory":"","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}
引用次数: 5
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