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2014-12-16
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idmasthead classsite-header rolebanner> div classsite-branding> h1 classsite-title>a hrefhttps://www.geolib.net/ titleGeolib.net relhome>Geolib.net/a>/h1> h2 classsite-description>Справочник по геологии/h2> /div>!-- .site-branding --> nav rolenavigation classsite-navigation main-navigation> h1 classassistive-text>Меню/h1> div classassistive-text skip-link>a href#content titleSkip to content>Skip to content/a>/div> div classmenu-glavnoe-menyu-container>ul idmenu-glavnoe-menyu classmenu>li idmenu-item-1101 classmenu-item menu-item-type-taxonomy menu-item-object-category menu-item-1101>a hrefhttps://www.geolib.net/mineralogy>Минералогия/a>/li> li idmenu-item-1102 classmenu-item menu-item-type-taxonomy menu-item-object-category menu-item-1102>a hrefhttps://www.geolib.net/petrography>Петрография/a>/li> li idmenu-item-1103 classmenu-item menu-item-type-taxonomy menu-item-object-category menu-item-1103>a hrefhttps://www.geolib.net/lithology>Литология/a>/li> li idmenu-item-1104 classmenu-item 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data-servicesvkontakte,facebook,odnoklassniki,moimir,gplus,twitter,pocket,telegram>/div> div idmain classsite-main> div idprimary classcontent-area> div idcontent classsite-content rolemain> article idpost-1991 classpost-1991 post type-post status-publish format-standard hentry category-tkrs> header classentry-header> h1 classentry-title>a relnofollow hrefhttps://www.geolib.net/tkrs/konservaciya-skvazhin.html relbookmark>Консервация скважин/a>/h1> div classentry-meta> a hrefhttps://www.geolib.net/tkrs/konservaciya-skvazhin.html relbookmark>time classentry-date >/time>/a> /div>!-- .entry-meta --> /header>!-- .entry-header --> div classentry-content> p styletext-align: justify;>Консервация скважин – комплекс мероприятий по своевременному предотвращению аварийных ситуаций и осложнений в скважинах, находящихся в бурении, законченных бурением и не подключенных к нефтесборной системе или остановленной (законсервированной) по каким-то технологическим или геологическим причинам в процессе эксплуатации. a hrefhttps://www.geolib.net/tkrs/konservaciya-skvazhin.html#more-1991 classmore-link>Читать далее/a>/p> /div>!-- .entry-content --> footer classentry-meta> span classcat-links> Рубрика: a hrefhttps://www.geolib.net/tkrs relcategory tag>Ремонт скважин/a> /span> /footer>!-- .entry-meta --> /article>!-- #post-1991 --> article idpost-1976 classpost-1976 post type-post status-publish format-standard hentry category-gis> header classentry-header> h1 classentry-title>a relnofollow hrefhttps://www.geolib.net/gis/bokovoy-karotazh.html relbookmark>Боковой каротаж/a>/h1> div classentry-meta> a hrefhttps://www.geolib.net/gis/bokovoy-karotazh.html relbookmark>time classentry-date >/time>/a> /div>!-- .entry-meta --> /header>!-- .entry-header --> div classentry-content> p styletext-align: justify;>Боковой каротаж, боковой микрокаротаж, боковое каротажное зондирование – часто используемые электрические методы геофизических исследований нефтяных и газовых скважин. a hrefhttps://www.geolib.net/gis/bokovoy-karotazh.html#more-1976 classmore-link>Читать далее/a>/p> /div>!-- .entry-content --> footer classentry-meta> span classcat-links> Рубрика: a hrefhttps://www.geolib.net/gis relcategory tag>ГИС/a> /span> /footer>!-- .entry-meta --> /article>!-- #post-1976 --> article idpost-1955 classpost-1955 post type-post status-publish format-standard hentry category-gis> header classentry-header> h1 classentry-title>a relnofollow hrefhttps://www.geolib.net/gis/ks-karotazh.html relbookmark>Каротаж сопротивления (КС)/a>/h1> div classentry-meta> a hrefhttps://www.geolib.net/gis/ks-karotazh.html relbookmark>time classentry-date >/time>/a> /div>!-- .entry-meta --> /header>!-- .entry-header --> div classentry-content> p styletext-align: justify;>Каротаж сопротивления (КС) – наряду с каротажем ПС распространенный электрический метод геофизических исследований скважин, только основан на изучении не естественных, а искусственных электрических полей. Метод показывает кажущееся удельное сопротивление пластов (Омм – ом*метр). a hrefhttps://www.geolib.net/gis/ks-karotazh.html#more-1955 classmore-link>Читать далее/a>/p> /div>!-- .entry-content --> footer classentry-meta> span classcat-links> Рубрика: a hrefhttps://www.geolib.net/gis relcategory tag>ГИС/a> /span> /footer>!-- .entry-meta --> /article>!-- #post-1955 --> article idpost-1928 classpost-1928 post type-post status-publish format-standard hentry category-gis> header classentry-header> h1 classentry-title>a relnofollow hrefhttps://www.geolib.net/gis/ps-karotazh.html relbookmark>Каротаж потенциала собственной поляризации (ПС)/a>/h1> div classentry-meta> a hrefhttps://www.geolib.net/gis/ps-karotazh.html relbookmark>time classentry-date >/time>/a> /div>!-- .entry-meta --> /header>!-- .entry-header --> div classentry-content> p alignjustify>Каротаж потенциала собственной поляризации (ПС) (англ. Spontaneous Potential log (SP)) – один из самых распространенных электрических методов геофизических исследований скважин, основанный на изучении естественных электрических полей. Показывает наличие естественных электрических полей возникающих благодаря протеканию на границах между породой и глинистым раствором электрохимических процессов (напряжение в мВ – милливольт). a hrefhttps://www.geolib.net/gis/ps-karotazh.html#more-1928 classmore-link>Читать далее/a>/p> /div>!-- .entry-content --> footer classentry-meta> span classcat-links> Рубрика: a hrefhttps://www.geolib.net/gis relcategory tag>ГИС/a> /span> /footer>!-- .entry-meta --> /article>!-- #post-1928 --> article idpost-1920 classpost-1920 post type-post status-publish format-standard hentry category-gis> header classentry-header> h1 classentry-title>a relnofollow hrefhttps://www.geolib.net/gis/impulsnyy-neytron-neytronnyy-karotazh.html relbookmark>Импульсный нейтрон-нейтронный каротаж/a>/h1> div classentry-meta> a hrefhttps://www.geolib.net/gis/impulsnyy-neytron-neytronnyy-karotazh.html relbookmark>time classentry-date >/time>/a> /div>!-- .entry-meta --> /header>!-- .entry-header --> div classentry-content> p alignjustify>Среди различных модификаций импульсных методов в нефтегазодобывающих предприятиях России наиболее распространённым является импульсный нейтрон-нейтронный каротаж (ИННК) (англ. Pulsed Neutron Logs (PNL). a hrefhttps://www.geolib.net/gis/impulsnyy-neytron-neytronnyy-karotazh.html#more-1920 classmore-link>Читать далее/a>/p> /div>!-- .entry-content --> footer classentry-meta> span classcat-links> Рубрика: a hrefhttps://www.geolib.net/gis relcategory tag>ГИС/a> /span> /footer>!-- .entry-meta --> /article>!-- #post-1920 --> article idpost-1914 classpost-1914 post type-post status-publish format-standard hentry category-gis> header classentry-header> h1 classentry-title>a relnofollow hrefhttps://www.geolib.net/gis/neytronnyy-gamma-karotazh.html relbookmark>Нейтронный гамма-каротаж/a>/h1> div classentry-meta> a hrefhttps://www.geolib.net/gis/neytronnyy-gamma-karotazh.html relbookmark>time classentry-date >/time>/a> /div>!-- .entry-meta --> /header>!-- .entry-header --> div classentry-content> p alignjustify>Нейтронный гамма-каротаж (НГК) (англ. Gamma Ray/Neutron Log (GNT)) основан на регистрации искусственно вызванного излучения γ-лучей, которое возникает при поглощении тепловых нейтронов ядрами химических элементов, входящих в состав той или иной горной породы, залегающей на данной глубине. Чем ниже плотность нейтронов, тем ниже регистрируемое вторичное γ-излучение. a hrefhttps://www.geolib.net/gis/neytronnyy-gamma-karotazh.html#more-1914 classmore-link>Читать далее/a>/p> /div>!-- .entry-content --> footer classentry-meta> span classcat-links> Рубрика: a hrefhttps://www.geolib.net/gis relcategory tag>ГИС/a> /span> /footer>!-- .entry-meta --> /article>!-- #post-1914 --> article idpost-1905 classpost-1905 post type-post status-publish format-standard hentry category-gis> header classentry-header> h1 classentry-title>a relnofollow hrefhttps://www.geolib.net/gis/akusticheskiy-karotazh.html relbookmark>Акустический каротаж/a>/h1> div classentry-meta> a hrefhttps://www.geolib.net/gis/akusticheskiy-karotazh.html relbookmark>time classentry-date >/time>/a> /div>!-- .entry-meta --> /header>!-- .entry-header --> div classentry-content> p alignjustify>Акустический каротаж (англ. Sonic Log) основан на разной скорости распространения упругих волн от источника к приёмнику прибора (V м/сек). a hrefhttps://www.geolib.net/gis/akusticheskiy-karotazh.html#more-1905 classmore-link>Читать далее/a>/p> /div>!-- .entry-content --> footer classentry-meta> span classcat-links> Рубрика: a hrefhttps://www.geolib.net/gis relcategory tag>ГИС/a> /span> /footer>!-- .entry-meta --> /article>!-- #post-1905 --> article idpost-1882 classpost-1882 post type-post status-publish format-standard hentry category-gis> header classentry-header> h1 classentry-title>a relnofollow hrefhttps://www.geolib.net/gis/gamma-karotazh.html relbookmark>Гамма-каротаж/a>/h1> div classentry-meta> a hrefhttps://www.geolib.net/gis/gamma-karotazh.html relbookmark>time classentry-date >/time>/a> /div>!-- .entry-meta --> /header>!-- .entry-header --> div classentry-content> p alignjustify>Гамма-каротаж (ГК) (англ. Gamma Ray Log (GR)) показывает естественную радиоактивность (или гамма-активность) пород в скважине, образуемую за счёт радиоактивных изотопов глинистых минералов: полевого шпата, слюды, иллита и минералов группы фосфатов. a hrefhttps://www.geolib.net/gis/gamma-karotazh.html#more-1882 classmore-link>Читать далее/a>/p> /div>!-- .entry-content --> footer classentry-meta> span classcat-links> Рубрика: a hrefhttps://www.geolib.net/gis relcategory tag>ГИС/a> /span> /footer>!-- .entry-meta --> /article>!-- #post-1882 --> article idpost-1854 classpost-1854 post type-post status-publish format-standard hentry category-mineralogy> header classentry-header> h1 classentry-title>a relnofollow hrefhttps://www.geolib.net/mineralogy/turmalin.html relbookmark>Турмалин/a>/h1> div classentry-meta> a hrefhttps://www.geolib.net/mineralogy/turmalin.html relbookmark>time classentry-date >/time>/a> /div>!-- .entry-meta --> /header>!-- .entry-header --> div classentry-content> p styletext-align: justify;>Турмалин (с сингал. තුරමලි “турамали” – драгоценный камень) – представитель группы минералов из класса алюмосиликатов переменного состава, содержащих в составе бор. Обобщенная химическая формула минерала выглядит примерно: Rsup>1+/sup>Rsup>2+/sup>sub>3/sub>Alsub>6/sub>Sisub>6/sub>Osub>18/sub>(BOsub>3/sub>)sub>3/sub>(OH)sub>4/sub>. Rsup>1+/sup> – ионы натрия или лития; Rsup>2+/sup> – ионы Mg, Fe, Mn./p> p styletext-align: justify;> a hrefhttps://www.geolib.net/mineralogy/turmalin.html#more-1854 classmore-link>Читать далее/a>/p> /div>!-- .entry-content --> footer classentry-meta> span classcat-links> Рубрика: a hrefhttps://www.geolib.net/mineralogy relcategory tag>Минералогия/a> /span> /footer>!-- .entry-meta --> /article>!-- #post-1854 --> article idpost-1839 classpost-1839 post type-post status-publish format-standard hentry category-mineralogy> header classentry-header> h1 classentry-title>a relnofollow hrefhttps://www.geolib.net/mineralogy/granat.html relbookmark>Гранат/a>/h1> div classentry-meta> a hrefhttps://www.geolib.net/mineralogy/granat.html relbookmark>time classentry-date >/time>/a> /div>!-- .entry-meta --> /header>!-- .entry-header --> div classentry-content> p styletext-align: justify;>Гранат – не существует минерала с таким названием. Гранатами называют целую группу минералов из класса силикатов. Название произошло из-за весьма большого сходства сростков кристаллов (щеток) с зернами фрукта граната. Общая химическая формула: Rsup>2+/sup>sub>3/sub>Rsup>3+/sup>sub>2/sub>(SiOsub>4/sub>)sub>3/sub>, где 2-хвалентным радикалом могут выступать Mg, Mn, Fe, Ca. 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