Automated Author Profile

Frey, Frederick A

0000-0002-5403-5677

Current S-Index

97.9

Sum of Dataset Indices for all datasets

Average Dataset Index per Dataset

1.7

Average Dataset Index per dataset

Total Datasets

58

Total datasets for this author

Average FAIR Score

93.6%

Average FAIR Score per dataset

Total Citations

91

Total citations to the author's datasets

Total Mentions

1

Total mentions of the author's datasets

S-Index Interpretation

S-Index Over Time

Cumulative Citations Over Time

Cumulative Mentions Over Time

Datasets

(Table S1) Major and minor element analyses of basaltic glasses from the Ninetyeast Ridge

No description available

Authors

  • Frey, Frederick A ;
  • Pringle, Malcolm S ;
  • Meleney, P ;
  • Huang, S ;
  • Piotrowski, Alexander M
0 Citations0 Mentions94% FAIR0.3 Dataset Index
10.1594/pangaea.7889192011

(Table S2) Trace element analyses of basaltic glasses from the Ninetyeast Ridge

No description available

Authors

  • Frey, Frederick A ;
  • Pringle, Malcolm S ;
  • Meleney, P ;
  • Huang, S ;
  • Piotrowski, Alexander M
0 Citations0 Mentions94% FAIR0.3 Dataset Index
10.1594/pangaea.7889202011

Minor-element chemical analyses of Hole 26-254

No description available

Authors

  • Frey, Frederick A ;
  • Davies, Thomas A ;
  • Luyendyk, Bruce P
0 Citations0 Mentions94% FAIR0.3 Dataset Index
10.1594/pangaea.2631232005

Minor-element chemical analyses of Hole 26-253

No description available

Authors

  • Frey, Frederick A ;
  • Davies, Thomas A ;
  • Luyendyk, Bruce P
0 Citations0 Mentions94% FAIR0.3 Dataset Index
10.1594/pangaea.2631222005

(Table S1) Age determination of Emperor Seamounts basement

The Hawaiian-Emperor hotspot track has a prominent bend, which has served as the basis for the theory that the Hawaiian hotspot, fixed in the deep mantle, traced a change in plate motion. However, paleomagnetic and radiometric age data from samples recovered by ocean drilling define an age-progressive paleolatitude history, indicating that the Emperor Seamount trend was principally formed by the rapid motion (over 40 millimeters per year) of the Hawaiian hotspot plume during Late Cretaceous to early-Tertiary times (81 to 47 million years ago). Evidence for motion of the Hawaiian plume affects models of mantle convection and plate tectonics, changing our understanding of terrestrial dynamics.

Authors

  • Tarduno, John A ;
  • Duncan, Robert A ;
  • Scholl, David W ;
  • Cottrell, Rory D ;
  • Steinberger, Bernhard ;
  • Thordarson, Thorvaldur ;
  • Kerr, Bryan C ;
  • Neal, Clive R ;
  • Frey, Frederick A ;
  • Torii, Masayuki ;
  • Carvallo, Claire
1 Citation0 Mentions88% FAIR1.3 Dataset Index
10.1594/pangaea.7721132003

(Table 2) Sr, Nd and Pb isotopic ratios in ODP Hole 183-1137A basaltic rocks

No description available

Authors

  • Ingle, Stephanie ;
  • Weis, Dominique A M ;
  • Scoates, James S ;
  • Frey, Frederick A
0 Citations0 Mentions96% FAIR2.1 Dataset Index
10.1594/pangaea.7109902002

(Table 1) Major and trace element concentrations of basaltic rocks from ODP Hole 183-1137A

No description available

Authors

  • Ingle, Stephanie ;
  • Weis, Dominique A M ;
  • Scoates, James S ;
  • Frey, Frederick A
0 Citations0 Mentions96% FAIR2.4 Dataset Index
10.1594/pangaea.7109892002

(Table 1) Sr-Nd-Pb isotopic compositions of samples from ODP Hole 183-1137

Basalts forming the floor of the Indian Ocean are geochemically distinct from those of the Atlantic and Pacific Oceans. These differences have been attributed to a deeply recycled continental component or to widespread dispersion of plume-type mantle within the Indian Ocean asthenosphere. The discovery of Proterozoic continental crustal rocks within the uppermost basaltic basement of Elan Bank, part of the Kerguelen Plateau, shows instead that direct shallow-level contamination of basaltic magmas by isolated continental crust fragments may have produced the anomalous isotopic ratios of some Indian Ocean basalts.

Authors

  • Weis, Dominique A M ;
  • Ingle, Stephanie ;
  • Damasceno, Dimitri ;
  • Frey, Frederick A ;
  • Nicolaysen, Kirsten P ;
  • Barling, Jane ;
  • Shipboard Scientific Party
0 Citations0 Mentions94% FAIR0.1 Dataset Index
10.1594/pangaea.7120872001

(Table 1) U-Pb isotopic results of single-grain zircon and monazite analyses, ODP Hole 183-1137A, Elan Bank

At Elan Bank of the Kerguelen Plateau in the southeast Indian Ocean, Leg 183 of the Ocean Drilling Program recovered clasts of garnet-biotite gneiss in a fluvial conglomerate intercalated with basalt flows. U-Pb and Pb-Pb dates of zircons and monazites in these clasts and an overlying sandstone range from 534 to 2547 Ma, which is much older than the surrounding Indian Ocean seafloor. These dates show that old continental crust resides in the shallow crust of the oceanic Kerguelen Plateau and that the breakup of Gondwana dispersed continental fragments into the nascent Indian Ocean lithosphere.

Authors

  • Nicolaysen, Kirsten P ;
  • Bowring, Samuel A ;
  • Frey, Frederick A ;
  • Weis, Dominique A M ;
  • Ingle, Stephanie ;
  • Pringle, Malcolm S ;
  • Coffin, Millard F
0 Citations1 Mention96% FAIR1.7 Dataset Index
10.1594/pangaea.7238962001

(Table 6) Isotope composition of lavas from ODP Site 119-738, Southern Kerguelen Plateau

No description available

Authors

  • Mahoney, John J ;
  • Jones, William B ;
  • Frey, Frederick A ;
  • Salters, Vincent J M ;
  • Pyle, Douglas G ;
  • Davies, Hugh L
0 Citations0 Mentions94% FAIR0.3 Dataset Index
10.1594/pangaea.7061131995