{"product_id":"turyshew-vqcheslaw-glinistye-mineraly-9786209395741","title":"Glinistye mineraly","description":"Cel'ü issledowaniq qwilos' rassmotrenie koncepcij proishozhdeniq glinistyh mineralow i wyqsnenie wozmozhnosti ih ispol'zowaniq w kachestwe indikatorow facial'no-klimaticheskih obstanowok i fiziko-himicheskih uslowij osadkonakopleniq w mezozojskih osadochnyh otlozheniqh Zapadno-Sibirskogo neftegazonosnogo megabassejna. V ürskih otlozheniqh dominiruüschimi qwlqütsq 4 glinistyh minerala - kaolinit, hlorit, gidroslüda i smeshannoslojnye obrazowaniq. V nizhnemelowyh otlozheniqh prisutstwuüt 5 glinistyh mineralow - kaolinit, hlorit, gidroslüda, smeshannoslojnye obrazowaniq i montmorillonit. V peschanikah sredneürskih otlozhenij preobladaet kaolinit, koncentriruüschijsq na wostoke central'noj chasti plity, i obratno korreliruüschij s gidroslüdoj, zanimaüschej zapadnuü oblast'. V peschanikah goteriw-barremskih otlozhenij preobladaet kaolinit, obratno korreliruüschij s hloritom. Glinistye mineraly w peschanikah berrias-walanzhinskogo wozrasta otrazhaüt fiziko-himicheskie uslowiq okruzhawshej ih sredy: mineralizaciü porowyh wod, znachenie pH, soderzhanie schelochnyh i schelochno-zemel'nyh älementow i t.d.","brand":"LAP LAMBERT Academic Publishing","offers":[{"title":"Default Title","offer_id":53812569145686,"sku":null,"price":0.0,"currency_code":"EUR","in_stock":false}],"thumbnail_url":"\/\/cdn.shopify.com\/s\/files\/1\/0925\/5829\/5382\/files\/product_image_9786209395741_1.jpg?v=1781817969","url":"https:\/\/www.momoxbooks.com\/products\/turyshew-vqcheslaw-glinistye-mineraly-9786209395741","provider":"momoxbooks","version":"1.0","type":"link"}