FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W3081133677> ?p ?o ?g. }

• W3081133677 endingPage "34" @default.
• W3081133677 startingPage "24" @default.
• W3081133677 abstract "A likely tuff bed lies along the gradational contact of the Middle and Upper Siwaliks in eastern Sulaiman Range, Taunsa area of Dera Ghazi Khan district, Pakistan. This tuffaceous unit is 0.5–3 m thick and extends for 10 km along the north-south strike in the eastern limb of the Zindapir anticline. It is greyish white to white on fresh surface, fine-grained to silty at the bottom and clayey at the top and thus shows a fining upward grain-size grading. The lower part of the ash bed shows a prominent lamination defined by megascopically visible abundant biotite, while the central and upper parts are so fine-grained that the individual minerals cannot be seen in hand sample. Unlike the lower well-laminated part, the central and upper parts are crudely laminated to apparently massive. The bulk samples analysed with X-ray diffraction consist of quartz, feldspar (plagioclase), biotite, clays, calcite and some ore mineral likely spinel, while the clay-size fractions contain illite, chlorite, biotite and probably their mixed-layered varieties. The colour, texture, presence of abundant biotite and stratigraphic position of the Taunsa tuff correlate with those reported from Potwar plateau and from Kashmir basin. However, the apparent absence of smectite from the XRD pattern makes the Taunsa ash bed different from both Potwar and Kashmir tuffs. The present stratigraphic position of the tuff bed corresponds to shallow diagenetic zone, while the absence of smectite in the tuff and crystallinity of illite suggest that the tuff is probably derived upon reworking from a deeper diagenetic zone belonging to a lower stratigraphic level. The Eocene or other older pre-Siwalik units in Pakistan may have or had some primary ashfall deposits as reported in the northwestern Himalayas of India. This older volcanic ash may have been reworked to its present site of occurrence along the gradational contact of the Middle and the Upper Siwaliks in Taunsa area of Dera Ghazi Khan. However, the primary source of the Taunsa tuff may belong more likely to Chagai arc in Pakistan than to Dacht-e-Nawar volcanic complex in Afghanistan." @default.
• W3081133677 created "2020-09-01" @default.
• W3081133677 creator A5002562477 @default.
• W3081133677 creator A5052272104 @default.
• W3081133677 creator A5062224282 @default.
• W3081133677 creator A5076503987 @default.
• W3081133677 creator A5088710004 @default.
• W3081133677 creator A5090018610 @default.
• W3081133677 creator A5090294944 @default.
• W3081133677 date "2020-07-06" @default.
• W3081133677 modified "2023-09-24" @default.
• W3081133677 title "Occurrence of a Likely Tuff Bed between the Middle and Upper Siwaliks, Taunsa area, Dera Ghazi Khan, Eastern Sulaiman Range, Pakistan" @default.
• W3081133677 cites W1569875495 @default.
• W3081133677 cites W1602342308 @default.
• W3081133677 cites W1983528709 @default.
• W3081133677 cites W1991962217 @default.
• W3081133677 cites W2003885151 @default.
• W3081133677 cites W2005478134 @default.
• W3081133677 cites W2008682353 @default.
• W3081133677 cites W2011682741 @default.
• W3081133677 cites W2014029226 @default.
• W3081133677 cites W2023997601 @default.
• W3081133677 cites W2027612146 @default.
• W3081133677 cites W2029768059 @default.
• W3081133677 cites W2033993178 @default.
• W3081133677 cites W2035424785 @default.
• W3081133677 cites W2052358768 @default.
• W3081133677 cites W2056755178 @default.
• W3081133677 cites W2068000204 @default.
• W3081133677 cites W2073235370 @default.
• W3081133677 cites W2101874561 @default.
• W3081133677 cites W2120950609 @default.
• W3081133677 cites W2126799938 @default.
• W3081133677 cites W2130849484 @default.
• W3081133677 cites W2135797186 @default.
• W3081133677 cites W2155975314 @default.
• W3081133677 cites W2271734648 @default.
• W3081133677 cites W2480549163 @default.
• W3081133677 cites W2512101538 @default.
• W3081133677 cites W2595171009 @default.
• W3081133677 cites W566475829 @default.
• W3081133677 cites W2181913428 @default.
• W3081133677 doi "https://doi.org/10.46660/ijeeg.vol11.iss1.2020.407" @default.
• W3081133677 hasPublicationYear "2020" @default.
• W3081133677 type Work @default.
• W3081133677 sameAs 3081133677 @default.
• W3081133677 citedByCount "1" @default.
• W3081133677 countsByYear W30811336772020 @default.
• W3081133677 crossrefType "journal-article" @default.
• W3081133677 hasAuthorship W3081133677A5002562477 @default.
• W3081133677 hasAuthorship W3081133677A5052272104 @default.
• W3081133677 hasAuthorship W3081133677A5062224282 @default.
• W3081133677 hasAuthorship W3081133677A5076503987 @default.
• W3081133677 hasAuthorship W3081133677A5088710004 @default.
• W3081133677 hasAuthorship W3081133677A5090018610 @default.
• W3081133677 hasAuthorship W3081133677A5090294944 @default.
• W3081133677 hasBestOaLocation W30811336771 @default.
• W3081133677 hasConcept C109007969 @default.
• W3081133677 hasConcept C114793014 @default.
• W3081133677 hasConcept C116637073 @default.
• W3081133677 hasConcept C127313418 @default.
• W3081133677 hasConcept C134306372 @default.
• W3081133677 hasConcept C151730666 @default.
• W3081133677 hasConcept C17409809 @default.
• W3081133677 hasConcept C199289684 @default.
• W3081133677 hasConcept C2777229588 @default.
• W3081133677 hasConcept C2777844515 @default.
• W3081133677 hasConcept C2778520076 @default.
• W3081133677 hasConcept C2779181077 @default.
• W3081133677 hasConcept C2779429093 @default.
• W3081133677 hasConcept C2779870107 @default.
• W3081133677 hasConcept C2780030769 @default.
• W3081133677 hasConcept C33923547 @default.
• W3081133677 hasConcept C40212044 @default.
• W3081133677 hasConceptScore W3081133677C109007969 @default.
• W3081133677 hasConceptScore W3081133677C114793014 @default.
• W3081133677 hasConceptScore W3081133677C116637073 @default.
• W3081133677 hasConceptScore W3081133677C127313418 @default.
• W3081133677 hasConceptScore W3081133677C134306372 @default.
• W3081133677 hasConceptScore W3081133677C151730666 @default.
• W3081133677 hasConceptScore W3081133677C17409809 @default.
• W3081133677 hasConceptScore W3081133677C199289684 @default.
• W3081133677 hasConceptScore W3081133677C2777229588 @default.
• W3081133677 hasConceptScore W3081133677C2777844515 @default.
• W3081133677 hasConceptScore W3081133677C2778520076 @default.
• W3081133677 hasConceptScore W3081133677C2779181077 @default.
• W3081133677 hasConceptScore W3081133677C2779429093 @default.
• W3081133677 hasConceptScore W3081133677C2779870107 @default.
• W3081133677 hasConceptScore W3081133677C2780030769 @default.
• W3081133677 hasConceptScore W3081133677C33923547 @default.
• W3081133677 hasConceptScore W3081133677C40212044 @default.
• W3081133677 hasIssue "1" @default.
• W3081133677 hasLocation W30811336771 @default.
• W3081133677 hasOpenAccess W3081133677 @default.
• W3081133677 hasPrimaryLocation W30811336771 @default.
• W3081133677 hasRelatedWork W11567808 @default.
• W3081133677 hasRelatedWork W15914952 @default.
• W3081133677 hasRelatedWork W16533376 @default.

• next