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Heavy mineral plot 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... -
Heavy mineral 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... -
Q-F-L-plot 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... -
Lithic composition 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... -
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... -
Sample position and type of analyses 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... -
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... -
Volumetric proportion of grains from the Nankai subduction zone (Japan) at IO...
Ternary diagrams are commonly used in Earth Sciences to represent numerical data as ratios of three components. For our study, ternary provenance diagrams were created in... -
Photomicrographs of representative mineralogy from the Nankai subduction zone...
Photomicrographs of representative mineralogy are here presented for each unit defined in our study. Unit A is dominated by quartz and feldspar whereas clay minerals,... -
Detrital zircon U/Pb ages from the Nankai subduction zone (Japan)
U-Pb zircon age dating was applied on U-channel samples (30cc) that were collected from sandy deposits in cores from IODP Site C0024 (one sample; frontal Nankai accretionary...
