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Bulk mineral composition on cores C00018, C0002D, C0002B and C0006E
This dataset has no description
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(Table 1) Composition of ODP Hole 107-652A samples
This dataset has no description
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(Table 2) Composition of ODP Hole 107-654A samples
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(Table 1) Detrital grains in five representative sandstone samples from the B...
This dataset has no description
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Gross composition of the Lanaittu Sandstone in Eastern Sardinia, Italy
The Lanaittu Sandstone (middle-upper Campanian, Eastern Sardinia, Italy) was analyzed using the point-counting technique to determine the composition and provenance of the... -
Detrital zircon geochronology data, petrographic point count data and paleocu...
Triassic turbidites of the Nanpanjiang basin of south China represent the most expansive and voluminous siliciclastic turbidite accumulation in south China. The Nanpanjiang... -
(Table T1) Mineral composition of turbidite sands and sandstones from ODP Leg...
During Ocean Drilling Program Leg 190 several turbidite successions in the Nankai Trough were drilled through including Pleistocene trench fill (Sites 1173 and 1174),... -
(Appendix) Mineral composition of ODP Leg 128 sandstone samples
Deep drilling in the Japan Sea during Legs 127 and 128 resulted in recovery of volcanic lithic sandstones from Leg 127, Sites 796 and 797, and feldspathic sandstones from Leg... -
Composition of Carnian to Norian sandstones from the Wombat Plateau (Table 1)
The Carnian to Norian sediments, as much as 600 m in total thickness, recovered from ODP Sites 759 and 760 on the Wombat Plateau, are generally represented by fluvial-dominated... -
(Table 1) Minerals at DSDP Hole 76-534A
A = abundant; C = common; P = present in small amounts; T = present as trace only. Analysis number = 20. -
(Table AT2) Petrology in point counts of ODP Hole 210-1276A, two ODP Leg 173 ...
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(Table 1) Detrital modes for sand grains in sediment core CRP-3
Detrital modes determined on 68 sandstone samples from CRP-3 drillcore indicate a continuation of the dynamic history of uplift-related erosion and unroofing previously... -
(Table 1) Detrital modes for sand grains in sediment core CRP-2/2A
Dynamic provenance variations are deduced from sand-grain detrital modes in samples obtained from the CRP-2/2A drillcore. Below an important unconformity at 307 metres below sea... -
(Table 1) Detrital modes for sand grains in sediment core CRP-1
Detrital modes for the sand-size fraction in 24 samples from the CRP-1 drillcore are described. Most samples are largely composed of quartzo-feldspathic detritus sourced... -
Modal analysis of Lanaittu Sandstone
The analyses of Lanaittu Sandstone (Campanian, Eastern Sardinia, Italy), recovered in a geognostic well in eastern Sardinia permit the reconstruction of the paleogeography of... -
Gravel petrology of Hudson strait sediments
Sediments from channel samples were weighed and sieved through a 2 mm mesh. Granules >2 mm were visually identified with a binocular microscope and dolomite was separated... -
(Table 1) Visual estimates of mineral and matrix percentages from AND1-1B thi...
In the original table, #0 is given as T. It is assumed here, that T means traces. However, the T is not explained in the article. -
(Table T3) Petrographic point-counts of turbidite sand deposits from ODP Leg ...
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(Table T2) Raw point-counts of volcaniclastic sands and sandstones from ODP L...
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Point-count analyses of grains from the Nankai subduction zone (Japan) at IOD...
For petrographic analyses, point counting was used to quantitatively estimate the modal composition of sand and sandstones by totalling the occurrence of various mineral grains...
