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all geography including DSDP/ODP Sites and Legs
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Africa
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Central Africa
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Gabon (1)
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East Africa
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Mozambique (1)
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Tanzania
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North Africa
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Algeria (2)
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Atlas Mountains
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Egypt
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Libya
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Rif
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Tunisia (1)
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Southern Africa
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Cenozoic
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Wanapum Basalt (1)
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Pliocene
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upper Pliocene
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Paleogene
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Eocene
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Willwood Formation (1)
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middle Eocene
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Tallahatta Formation (1)
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upper Eocene
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Priabonian (2)
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Hanna Formation (1)
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Oligocene
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Chattian (4)
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Paleocene
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Danian (3)
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K-T boundary (1)
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Pysht Formation (1)
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upper Cenozoic (1)
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Mesozoic
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Cretaceous
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Colorado Group (2)
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Lower Cretaceous
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Albian
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Mancos Shale (1)
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Lower Jurassic
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Posidonia Shale (1)
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Upper Jurassic
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Arab Formation (1)
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Kimmeridgian
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lower Kimmeridgian (1)
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Morrison Formation (2)
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Oxfordian
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upper Oxfordian (1)
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Salt Wash Sandstone Member (1)
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Navajo Sandstone (1)
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Permian-Triassic boundary (5)
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Middle Triassic
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Ischigualasto Formation (1)
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Norian (1)
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Sag River Sandstone (1)
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Paleozoic
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Cambrian
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Upper Cambrian
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Galesville Sandstone (1)
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Carboniferous
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Hartselle Sandstone (1)
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Salem Limestone (1)
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Pennsylvanian
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Brazil Formation (1)
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Minturn Formation (1)
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Virgilian
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-
-
-
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Devonian
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Old Red Sandstone (1)
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Palliser Formation (1)
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Ordovician
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Fillmore Formation (1)
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Middle Ordovician
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Platteville Formation (1)
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Upper Ordovician
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Kope Formation (1)
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Sandbian (1)
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Wufeng Formation (1)
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-
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Permian
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Blaine Formation (1)
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Guadalupian
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Capitanian (1)
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Roadian (1)
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Tansill Formation (1)
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Lower Permian
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Cisuralian
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Leonardian (2)
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Middle Permian (2)
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Rotliegendes (2)
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Devonian
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GeoRef Categories
Era and Period
Epoch and Age
Book Series
Date
Availability
log-spiral
(A) Mbotyi Bay, here a half-graben is being excavated out as a log-spiral ... Available to Purchase
The typical log-spiral morphology and location of the two strandline deposi... Available to Purchase
Comparison between limit-equilibrium method (slices, circle, log-spiral, an... Available to Purchase
Submarine mass flow channels as an underlying control for headland-bound embayments, southeast African coastline Available to Purchase
Safety Number Calculated by Different Methods and for Different Failure Sur... Available to Purchase
Paleogeography of the Lonesome Point, Michigan, USA, strandplain complex fr... Available to Purchase
Key elements illustrating the genetic development ofa coastal heavy mineral... Available to Purchase
The logarithmic spiral; definition and expression of a new graphical representation of results in sedimentological analysis Available to Purchase
Relationship between growth rate and supersaturation for fluorapatite plott... Available to Purchase
Morphological characteristics of illitic clay minerals from a hydrothermal system Available to Purchase
Coalbed Methane Applications of Wireline Logs Available to Purchase
Abstract Valuable geologic information can be obtained by utilizing wireline conveyed measurements. Generally referred to as “logs," these readings probably derive their name from the general term meaning a “record" of a series of events. In the context used here, the term log refers to a particular measurement in a well that is recorded as a function of well depth. It often refers to a measurement of one or more physical properties as a function of well depth. From these physical properties, the rock properties are inferred. Results are not limited to rock property measurements, though. Examples of other types of logs are fluid flow, cement quality, casing corrosion, etc. Having defined the term log , why the term wireline? This is to differentiate between logs made from instruments lowered into the well on a cable, and logs made in the oil field by noncable means such as mud logs (drilling mud characteristics), drilling time logs (bit penetration rates), etc. The term cable, as used in the foregoing comment, should be clarified. Cables, in their most familiar form, are strong, flexible "ropes" made of spiraled metal strands. "Wireline" denotes a special form of metal stranded cable that contains electrical conductors on the inside (core). These conductors generally serve dual purposes: to power the downhole instrument (tool) and to convey the tool signal back to the surface for display on the log. The "wireline" cable causes some difficult obstacles for the logging service company. Because of the small diameter conductors, line resistance tends