FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W2321885448> ?p ?o ?g. }

• W2321885448 endingPage "264" @default.
• W2321885448 startingPage "227" @default.
• W2321885448 abstract "The author has been studying on clay minerals in the oil-hearing Neogene Tertiary sedimentary rocks of Northwest Honshû, Japan. In this paper he describes his provisional criteria for analysis of clay minerals in sedimentary rocks, with his basic considerations and laboratory experiments, which he conducted. He adds supplementary notes on the qualitative analysis to his preceding paper20). He also summarizes some noteworthy sedimentological relations, which have been considered by him to exist in sedimentary sequences of many geological basins. Contents of this paper are as follows: 1) Progress of basic experiments for the establishment of the criteria and some result of qualitative analysis are described. a) X-ray diffraction analysis applied to centrifugal fractions of mudstones due to random powder method. b) X-ray diffraction analysis combined with various reagent-treatments and heat-treatment, applied to centrifugal fractions of mudstones due to powder orientation method. 2) He determined clay mineral suit of montmorillonite-illite-chlorite (± minor amount of montmorillonite-illite mixed layer), for the oil-bearing Neogene Tertiary sedimentary rocks in Northwest Honshû, Japan. 3) He proposed a classification of mudstones due to relative amount of clay minerals and quartz. 4) He found the striking negative correlation between the montmorillonite log (or clay mineral log) and the log of “Cl'-concentration of interstitial water” in mudstones, prepared for the exploration well Mitsuke SK. 1 (or Tamugiyama SK. 1). Based on consideration of it, he interpreted that a part of the so-called interstitial water, is composed of that delivered from interlayer water of montmorillonite crystals, through the pretreatment or heating up to 110°C of core samples. This interpretation is supported by the result of another experiment of his own, in which the oscillation method of X-ray diffraction analysis during heating up to 900°C, is applied to a centrifugal fraction of a mudstone cored from the depth of 1098m of the well Tamugiyama SK. 1. 5) The author determined clay-mineralogical divisions on the montmorillonite log, and he found that these divisions coincide with fossil foraminiferal subzonules. 6) On the Q-M (quartz-montmorillonite) diagrams characteristic distribution curve can be drawn for each fossil foraminiferal biotope unit in the Mitsuke and Tamugiyama sections. Existence of a kind of sedimentological relation is suggested by the comparison of relative positions of these characteristic distribution curves on Q-M diagrams with their corresponding foraminiferal faunal assemblages. 7) The author describes the possibility to determine characteristic distribution curves on the M-I-Chl (montmorillonite-illite-chlorite) triangular diagrams for geological formations or members. 8) The criteria for analysis of clay minerals in sedimentary rocks, which he proposed, are described. 9) In conclusion, present status and future problems of the sedimentary clay mineralogy, especially that concerning petroleum exploration and exploitation, are summarized." @default.
• W2321885448 created "2016-06-24" @default.
• W2321885448 creator A5069240986 @default.
• W2321885448 date "1962-01-01" @default.
• W2321885448 modified "2023-10-01" @default.
• W2321885448 title "Studies on Clay Minerals in the Oil-bearing Neogene Tertiary Sedimentary Rocks of Northwest Honshû, Japan, with a Proposal of Criteria for Analysis of Clay Minerals in Sedimentary Rocks" @default.
• W2321885448 doi "https://doi.org/10.3720/japt.27.227" @default.
• W2321885448 hasPublicationYear "1962" @default.
• W2321885448 type Work @default.
• W2321885448 sameAs 2321885448 @default.
• W2321885448 citedByCount "2" @default.
• W2321885448 countsByYear W23218854482016 @default.
• W2321885448 crossrefType "journal-article" @default.
• W2321885448 hasAuthorship W2321885448A5069240986 @default.
• W2321885448 hasBestOaLocation W23218854481 @default.
• W2321885448 hasConcept C109007969 @default.
• W2321885448 hasConcept C114793014 @default.
• W2321885448 hasConcept C127313418 @default.
• W2321885448 hasConcept C151730666 @default.
• W2321885448 hasConcept C17409809 @default.
• W2321885448 hasConcept C178790620 @default.
• W2321885448 hasConcept C185592680 @default.
• W2321885448 hasConcept C199289684 @default.
• W2321885448 hasConcept C27492601 @default.
• W2321885448 hasConcept C2777515222 @default.
• W2321885448 hasConcept C2777844515 @default.
• W2321885448 hasConcept C2779429093 @default.
• W2321885448 hasConcept C2779870107 @default.
• W2321885448 hasConcept C40212044 @default.
• W2321885448 hasConcept C6494504 @default.
• W2321885448 hasConceptScore W2321885448C109007969 @default.
• W2321885448 hasConceptScore W2321885448C114793014 @default.
• W2321885448 hasConceptScore W2321885448C127313418 @default.
• W2321885448 hasConceptScore W2321885448C151730666 @default.
• W2321885448 hasConceptScore W2321885448C17409809 @default.
• W2321885448 hasConceptScore W2321885448C178790620 @default.
• W2321885448 hasConceptScore W2321885448C185592680 @default.
• W2321885448 hasConceptScore W2321885448C199289684 @default.
• W2321885448 hasConceptScore W2321885448C27492601 @default.
• W2321885448 hasConceptScore W2321885448C2777515222 @default.
• W2321885448 hasConceptScore W2321885448C2777844515 @default.
• W2321885448 hasConceptScore W2321885448C2779429093 @default.
• W2321885448 hasConceptScore W2321885448C2779870107 @default.
• W2321885448 hasConceptScore W2321885448C40212044 @default.
• W2321885448 hasConceptScore W2321885448C6494504 @default.
• W2321885448 hasIssue "6" @default.
• W2321885448 hasLocation W23218854481 @default.
• W2321885448 hasOpenAccess W2321885448 @default.
• W2321885448 hasPrimaryLocation W23218854481 @default.
• W2321885448 hasRelatedWork W1987489095 @default.
• W2321885448 hasRelatedWork W2001317829 @default.
• W2321885448 hasRelatedWork W2058852830 @default.
• W2321885448 hasRelatedWork W2060481564 @default.
• W2321885448 hasRelatedWork W2321885448 @default.
• W2321885448 hasRelatedWork W2352175373 @default.
• W2321885448 hasRelatedWork W2357557092 @default.
• W2321885448 hasRelatedWork W2367171600 @default.
• W2321885448 hasRelatedWork W2187789352 @default.
• W2321885448 hasRelatedWork W2188606304 @default.
• W2321885448 hasVolume "27" @default.
• W2321885448 isParatext "false" @default.
• W2321885448 isRetracted "false" @default.
• W2321885448 magId "2321885448" @default.
• W2321885448 workType "article" @default.