FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W2045835314> ?p ?o ?g. }

• W2045835314 abstract "The Northwest Hartburg field, located in southern Newton County, Texas, is in a structural belt which forms part of the Gulf Coast Frio (Oligocene-Miocene) producing trend and for which the name Hartburg flexure is suggested. The various structural and depositional features (folds, faults, truncation, channels, etc.) observed in this trend are particularly well exhibited in the Northwest Hartburg field area and indicate a structural development which, reaching a climax during earlier Frio time, can be divided into four stages. Stage 1: During stage 1, continental shelf conditions prevailed throughout the area and a sedimentary series, consisting essentially of shale in its and a sandy section in its upper part, was deposited on the slowly subsiding shelf. The sand section is subdivided, in ascending order, into the Nodosaria sand, and and upper Hartburg sands, the latter two names replacing the more commonly used but misleading names lower and upper Hackberry sands. Stage 2: Toward the end of upper Hartburg sand sedimentation, the area experienced a large scale and semi-regional structural disturbance in the form of a breakdown of a segment of the Gulf Coast geosynclinal floor. This event tilted the continental shelf, producing the Hartburg flexure (scarp) and an embayment which was later filled by the Hackberry shale. Stage 3: The tilting of the continental shelf area induced gravity flow in the sedimentary beds which was essentially a downfolding process. The resulting synclinal folds formed deep troughs and trenches turning the scarp into one of considerable relief that resembled the topography of the present continental slope of the northwestern Gulf of Mexico. Most of the troughs show effects of local submarine erosion in the form of channels and scour scars, some of which extended also across the anticlinal fold adjoining the trough. Besides tilting the continental shelf, the regional downwarp also lowered the base level of erosion and depositions across the shelf area. In adjustment to the new profile of equilibrium the anticlinal folds were truncated as evidenced by the presence of a local angular uncon ormity between the Hackberry shale and underlying formations. Stage 4: After gravity flow subsided and the new base level of erosion was attained, turbidity currents and sedimentary flows filled the troughs and channels with channel-fill deposits. On completion of the peneplaning action, the deposition of the Hackberry shale commenced restoring again to the area more normal depositional conditions. Mild folding and faulting continued or were rejuvenated during this and later depositional cycles on some of the local folds in the Hartburg trend." @default.
• W2045835314 created "2016-06-24" @default.
• W2045835314 creator A5007859735 @default.
• W2045835314 date "1960-01-01" @default.
• W2045835314 modified "2023-09-26" @default.
• W2045835314 title "Depositional and Structural History of Northwest Hartburg Field, Newton County, Texas" @default.
• W2045835314 cites W1565983386 @default.
• W2045835314 cites W1980941728 @default.
• W2045835314 cites W2130940357 @default.
• W2045835314 cites W2147052644 @default.
• W2045835314 cites W2165485216 @default.
• W2045835314 cites W2170492852 @default.
• W2045835314 cites W2601390057 @default.
• W2045835314 doi "https://doi.org/10.1306/0bda5fff-16bd-11d7-8645000102c1865d" @default.
• W2045835314 hasPublicationYear "1960" @default.
• W2045835314 type Work @default.
• W2045835314 sameAs 2045835314 @default.
• W2045835314 citedByCount "7" @default.
• W2045835314 crossrefType "journal-article" @default.
• W2045835314 hasAuthorship W2045835314A5007859735 @default.
• W2045835314 hasConcept C109007969 @default.
• W2045835314 hasConcept C126753816 @default.
• W2045835314 hasConcept C127313418 @default.
• W2045835314 hasConcept C151730666 @default.
• W2045835314 hasConcept C16674752 @default.
• W2045835314 hasConcept C166957645 @default.
• W2045835314 hasConcept C202444582 @default.
• W2045835314 hasConcept C205649164 @default.
• W2045835314 hasConcept C33923547 @default.
• W2045835314 hasConcept C9652623 @default.
• W2045835314 hasConceptScore W2045835314C109007969 @default.
• W2045835314 hasConceptScore W2045835314C126753816 @default.
• W2045835314 hasConceptScore W2045835314C127313418 @default.
• W2045835314 hasConceptScore W2045835314C151730666 @default.
• W2045835314 hasConceptScore W2045835314C16674752 @default.
• W2045835314 hasConceptScore W2045835314C166957645 @default.
• W2045835314 hasConceptScore W2045835314C202444582 @default.
• W2045835314 hasConceptScore W2045835314C205649164 @default.
• W2045835314 hasConceptScore W2045835314C33923547 @default.
• W2045835314 hasConceptScore W2045835314C9652623 @default.
• W2045835314 hasLocation W20458353141 @default.
• W2045835314 hasOpenAccess W2045835314 @default.
• W2045835314 hasPrimaryLocation W20458353141 @default.
• W2045835314 hasRelatedWork W1937777925 @default.
• W2045835314 hasRelatedWork W2001197856 @default.
• W2045835314 hasRelatedWork W2030818517 @default.
• W2045835314 hasRelatedWork W2073779914 @default.
• W2045835314 hasRelatedWork W2103355267 @default.
• W2045835314 hasRelatedWork W2186171420 @default.
• W2045835314 hasRelatedWork W2332067357 @default.
• W2045835314 hasRelatedWork W2750126329 @default.
• W2045835314 hasRelatedWork W3120602938 @default.
• W2045835314 hasRelatedWork W3139698491 @default.
• W2045835314 hasVolume "44" @default.
• W2045835314 isParatext "false" @default.
• W2045835314 isRetracted "false" @default.
• W2045835314 magId "2045835314" @default.
• W2045835314 workType "article" @default.