Skip to main navigation
Skip to search
Skip to main content
Penn State Home
Help & FAQ
Home
Researchers
Research output
Research units
Equipment
Grants & Projects
Prizes
Activities
Search by expertise, name or affiliation
Temporal patterns among Phanerozoic oolitic ironstones and oceanic anoxia
F. B. Van Houten, M. A. Arthur
Geosciences
Research output
:
Contribution to journal
›
Article
›
peer-review
80
Scopus citations
Overview
Fingerprint
Fingerprint
Dive into the research topics of 'Temporal patterns among Phanerozoic oolitic ironstones and oceanic anoxia'. Together they form a unique fingerprint.
Sort by
Weight
Alphabetically
Keyphrases
Temporal Patterns
100%
Phanerozoic
100%
Oceanic Anoxia
100%
Black Shale
60%
Transgression
20%
Ordovician
20%
Submergence
20%
Sequence Scales
20%
Recurring
10%
Phase Lead
10%
Rate of Change
10%
Erosion Rate
10%
Oxygenation
10%
Cratonic
10%
Global Climate Change
10%
Water Masses
10%
Deep Water Masses
10%
Quasi-periodic
10%
Sedimentation Rate
10%
Subsidence
10%
Sedimentary Rocks
10%
Organic-rich
10%
Unconformity
10%
Cratons
10%
Craton Margin
10%
Regional Unconformity
10%
Foreland Basin
10%
Stratigraphic Distribution
10%
Epicontinental Sea
10%
Local Development
10%
Sediment Supply
10%
Asymmetric Unit
10%
Palaeogene
10%
Earth and Planetary Sciences
Ironstone
100%
Detrital Deposit
8%
Jurassic Period
8%
Intracratonic Basin
8%
Local Development
8%
Ordovician Period
8%