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Autori principali: Bramlette, M, Faughn, James L, Hurley, RJ
Natura: Dataset Open Access
Lingua:en
Pubblicazione: PANGAEA 1959
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Accesso online:https://doi.org/10.1594/PANGAEA.857399
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author Bramlette, M
Faughn, James L
Hurley, RJ
author_facet Bramlette, M
Faughn, James L
Hurley, RJ
collection Datos científicos de ciencias marinas y ambientales
contents Some short cores from the shelf at about 800-1000 fathoms on the southwest flank of Eniwetok Atoll penetrated Pliocene deposits with little to no later sediment cover. The Quaternary deposits include much coarse reef debris, particularly the fragments of algae such as Halimeda and other shallow-water material up to several millimeters in grain size, mixed with varying amounts of pelagic Foraminifera. The Pliocene sediments (one may be upper Miocene) are pure pelagic deposits of much finer grain size, consisting of coccoliths and pelagic Foraminifera with no admixture of reef material. Bottom photographs show areas of well-developed ripple marks in coarse sediment (C. J. Shipek, manuscript) apparently formed only in the areas with the veneer of post-Tertiary coarse sediments. A brown impregnation at the top and extending down as mottling for a few centimeters is also usual in the Tertiary sediment of the cores. This seems to consist of iron and manganese oxides and adds somewhat to the induration.
format Dataset Open Access
id pangaea_https___doi_org_10_1594_PANGAEA_857399
institution PANGAEA
language en
publishDate 1959
publisher PANGAEA
record_format pangaea
spellingShingle Annotated record of the detailed examination of Mn deposits of the Eniwetok Atoll
Bramlette, M
Faughn, James L
Hurley, RJ
10-J1268; 10-J1269; 10-J1270; 10-J1271; 10-J1272; 10-J1273; 10-J1274; 10-J1275; 11-J1276; 3-J1225; 3-J1226; 3-J1227; 3-J1228; 4-J1230; 4-J1231; 4-J1232; 4-J1233; 4-J1234; 4-J1235; 6-J1237; 6-J1238; 6-J1239; 6-J1240; 6-J1241; 6-J1242; 6-J1243; 6-J1244; 8-J1260; 8-J1261; 8-J1262; 8-J1263; 8-J1264; 8-J1265; 8-J1266; Comment; Core; CORE; Deposit type; DEPTH, sediment/rock; Description; Elevation of event; ENIW10PH-1268; ENIW10PH-1269; ENIW10PH-1270; ENIW10PH-1271; ENIW10PH-1272; ENIW10PH-1273; ENIW10PH-1274; ENIW10PH-1275; ENIW11PH-1276; ENIW20C; ENIW27C; ENIW3PH-1225; ENIW3PH-1226; ENIW3PH-1227; ENIW3PH-1228; ENIW4C; ENIW4PH-1230; ENIW4PH-1231; ENIW4PH-1232; ENIW4PH-1233; ENIW4PH-1234; ENIW4PH-1235; ENIW6PH-1237; ENIW6PH-1238; ENIW6PH-1239; ENIW6PH-1240; ENIW6PH-1241; ENIW6PH-1242; ENIW6PH-1243; ENIW6PH-1244; ENIW8PH-1260; ENIW8PH-1261; ENIW8PH-1262; ENIW8PH-1263; ENIW8PH-1264; ENIW8PH-1265; ENIW8PH-1266; ENIWETOK_Operation; Eniwetok Atoll, Central Pacific; Event label; H.M. Smith; Latitude of event; Longitude of event; NOAA and MMS Marine Minerals Geochemical Database; NOAA-MMS; Photo/Video; Position; PV; Quantity of deposit; Sample ID; Sediment type; Size; Substrate type; Uniform resource locator/link to image
Some short cores from the shelf at about 800-1000 fathoms on the southwest flank of Eniwetok Atoll penetrated Pliocene deposits with little to no later sediment cover. The Quaternary deposits include much coarse reef debris, particularly the fragments of algae such as Halimeda and other shallow-water material up to several millimeters in grain size, mixed with varying amounts of pelagic Foraminifera. The Pliocene sediments (one may be upper Miocene) are pure pelagic deposits of much finer grain size, consisting of coccoliths and pelagic Foraminifera with no admixture of reef material. Bottom photographs show areas of well-developed ripple marks in coarse sediment (C. J. Shipek, manuscript) apparently formed only in the areas with the veneer of post-Tertiary coarse sediments. A brown impregnation at the top and extending down as mottling for a few centimeters is also usual in the Tertiary sediment of the cores. This seems to consist of iron and manganese oxides and adds somewhat to the induration.
title Annotated record of the detailed examination of Mn deposits of the Eniwetok Atoll
topic 10-J1268; 10-J1269; 10-J1270; 10-J1271; 10-J1272; 10-J1273; 10-J1274; 10-J1275; 11-J1276; 3-J1225; 3-J1226; 3-J1227; 3-J1228; 4-J1230; 4-J1231; 4-J1232; 4-J1233; 4-J1234; 4-J1235; 6-J1237; 6-J1238; 6-J1239; 6-J1240; 6-J1241; 6-J1242; 6-J1243; 6-J1244; 8-J1260; 8-J1261; 8-J1262; 8-J1263; 8-J1264; 8-J1265; 8-J1266; Comment; Core; CORE; Deposit type; DEPTH, sediment/rock; Description; Elevation of event; ENIW10PH-1268; ENIW10PH-1269; ENIW10PH-1270; ENIW10PH-1271; ENIW10PH-1272; ENIW10PH-1273; ENIW10PH-1274; ENIW10PH-1275; ENIW11PH-1276; ENIW20C; ENIW27C; ENIW3PH-1225; ENIW3PH-1226; ENIW3PH-1227; ENIW3PH-1228; ENIW4C; ENIW4PH-1230; ENIW4PH-1231; ENIW4PH-1232; ENIW4PH-1233; ENIW4PH-1234; ENIW4PH-1235; ENIW6PH-1237; ENIW6PH-1238; ENIW6PH-1239; ENIW6PH-1240; ENIW6PH-1241; ENIW6PH-1242; ENIW6PH-1243; ENIW6PH-1244; ENIW8PH-1260; ENIW8PH-1261; ENIW8PH-1262; ENIW8PH-1263; ENIW8PH-1264; ENIW8PH-1265; ENIW8PH-1266; ENIWETOK_Operation; Eniwetok Atoll, Central Pacific; Event label; H.M. Smith; Latitude of event; Longitude of event; NOAA and MMS Marine Minerals Geochemical Database; NOAA-MMS; Photo/Video; Position; PV; Quantity of deposit; Sample ID; Sediment type; Size; Substrate type; Uniform resource locator/link to image
url https://doi.org/10.1594/PANGAEA.857399