Automated Author ProfileMeyer, Peter S
Meyer, Peter S
Current S-Index
Sum of Dataset Indices for all datasets
Average Dataset Index per Dataset
Average Dataset Index per dataset
Total Datasets
Total datasets for this author
Average FAIR Score
Average FAIR Score per dataset
Total Citations
Total citations to the author's datasets
Total Mentions
Total mentions of the author's datasets
S-Index Interpretation
The S-Index (Sharing Index) is a comprehensive metric that represents the cumulative impact of all your datasets. It is calculated as the sum of Dataset Index scores across all your claimed datasets.
What it means:
- A higher S-index indicates greater overall impact of your datasets relative to typical datasets in their fields of research
- The S-Index grows as you add more datasets or as existing datasets gain more citations and mentions
- It provides a single number to track your research data impact over time
Current S-Index: 25.9 (sum of 26 datasets Dataset Index scores)
More information here.
S-Index Over Time
Cumulative Citations Over Time
Cumulative Mentions Over Time
Datasets
No description available
Authors
- Dick, Henry J B ;
- Ozawa, Kazuhito ;
- Meyer, Peter S ;
- Niu, Yaoling ;
- Robinson, Paul T ;
- Constantin, Marc ;
- Hébert, Rejean ;
- Maeda, Jinichiro ;
- Natland, James H ;
- Hirth, James Gregory ;
- Mackie, Suzie
No description available
Authors
- Dick, Henry J B ;
- Ozawa, Kazuhito ;
- Meyer, Peter S ;
- Niu, Yaoling ;
- Robinson, Paul T ;
- Constantin, Marc ;
- Hébert, Rejean ;
- Maeda, Jinichiro ;
- Natland, James H ;
- Hirth, James Gregory ;
- Mackie, Suzie
No description available
Authors
- Dick, Henry J B ;
- Ozawa, Kazuhito ;
- Meyer, Peter S ;
- Niu, Yaoling ;
- Robinson, Paul T ;
- Constantin, Marc ;
- Hébert, Rejean ;
- Maeda, Jinichiro ;
- Natland, James H ;
- Hirth, James Gregory ;
- Mackie, Suzie
No description available
Authors
- Dick, Henry J B ;
- Ozawa, Kazuhito ;
- Meyer, Peter S ;
- Niu, Yaoling ;
- Robinson, Paul T ;
- Constantin, Marc ;
- Hébert, Rejean ;
- Maeda, Jinichiro ;
- Natland, James H ;
- Hirth, James Gregory ;
- Mackie, Suzie
No description available
Authors
- Dick, Henry J B ;
- Ozawa, Kazuhito ;
- Meyer, Peter S ;
- Niu, Yaoling ;
- Robinson, Paul T ;
- Constantin, Marc ;
- Hébert, Rejean ;
- Maeda, Jinichiro ;
- Natland, James H ;
- Hirth, James Gregory ;
- Mackie, Suzie
Ocean Drilling Program Leg 176 deepened Hole 735B in gabbroic lower ocean crust by 1 km to 1.5 km. The section has the physical properties of seismic layer 3, and a total magnetization sufficient by itself to account for the overlying lineated sea-surface magnetic anomaly. The rocks from Hole 735B are principally olivine gabbro, with evidence for two principal and many secondary intrusive events. There are innumerable late small ferrogabbro intrusions, often associated with shear zones that cross-cut the olivine gabbros. The ferrogabbros dramatically increase upward in the section. Whereas there are many small patches of ferrogabbro representing late iron- and titanium-rich melt trapped intragranularly in olivine gabbro, most late melt was redistributed prior to complete solidification by compaction and deformation. This, rather than in situ upward differentiation of a large magma body, produced the principal igneous stratigraphy. The computed bulk composition of the hole is too evolved to mass balance mid-ocean ridge basalt back to a primary magma, and there must be a significant mass of missing primitive cumulates. These could lie either below the hole or out of the section. Possibly the gabbros were emplaced by along-axis intrusion of moderately differentiated melts into the near-transform environment. Alteration occurred in three stages. High-temperature granulite- to amphibolite-facies alteration is most important, coinciding with brittle-ductile deformation beneath the ridge. Minor greenschist-facies alteration occurred under largely static conditions, likely during block uplift at the ridge transform intersection. Late post-uplift low-temperature alteration produced locally abundant smectite, often in previously unaltered areas. The most important features of the high- and low-temperature alteration are their respective associations with ductile and cataclastic deformation, and an overall decrease downhole with hydrothermal alteration generally <=5% in the bottom kilometer. Hole 735B provides evidence for a strongly heterogeneous lower ocean crust, and for the inherent interplay of deformation, alteration and igneous processes at slow-spreading ridges. It is strikingly different from gabbros sampled from fast-spreading ridges and at most well-described ophiolite complexes. We attribute this to the remarkable diversity of tectonic environments where crustal accretion occurs in the oceans and to the low probability of a section of old slow-spread crust formed near a major large-offset transform being emplaced on-land compared to sections of young crust from small ocean basins.
Authors
- Dick, Henry J B ;
- Natland, James H ;
- Alt, Jeffrey C ;
- Bach, Wolfgang ;
- Bideau, Daniel ;
- Gee, Jeff S ;
- Haggas, Sarah L ;
- Hertogen, Jan GH ;
- Hirth, James Gregory ;
- Holm, Paul Martin ;
- Ildefonse, Benoit ;
- Iturrino, Gerardo J ;
- John, Barbara E ;
- Kelley, Deborah S ;
- Kikawa, Eiichi ;
- Kingdon, Andrew ;
- LeRoux, Petrus J ;
- Maeda, Jinichiro ;
- Meyer, Peter S ;
- Miller, D Jay ;
- Naslund, Howard Richard ;
- Niu, Yaoling ;
- Robinson, Paul T ;
- Snow, Jonathan E ;
- Stephen, Ralph A ;
- Trimby, Patrick W ;
- Worm, Horst-Ulrich ;
- Yoshinobu, Aaron
No description available
Authors
- Hart, Stanley R ;
- Blusztajn, Jerzy S ;
- Dick, Henry J B ;
- Meyer, Peter S ;
- Muehlenbachs, Karlis
No description available
Authors
- Hart, Stanley R ;
- Blusztajn, Jerzy S ;
- Dick, Henry J B ;
- Meyer, Peter S ;
- Muehlenbachs, Karlis
No description available
Authors
- Hart, Stanley R ;
- Blusztajn, Jerzy S ;
- Dick, Henry J B ;
- Meyer, Peter S ;
- Muehlenbachs, Karlis