Earth: Day Zero • Paper 166 of 512
Central Atlantic Magmatic Province
The Central Atlantic Magmatic Province, or CAMP, is one of the largest known magmatic provinces associated with continental breakup.
Regional Geological Context
CAMP-related rocks occur across eastern North America, northern South America, western Africa, and southwestern Europe, including regions associated with Nova Scotia, Canada; New Jersey, United States; Morocco; Portugal; and Brazil.
Relevant institutions include Rutgers University in New Brunswick, New Jersey, United States; Dalhousie University in Halifax, Nova Scotia, Canada; and University of Lisbon in Lisbon, Portugal.
Observation
CAMP preserves volcanic and intrusive systems distributed across formerly connected continental margins.
Constraint Analysis
Its distribution provides a useful test case for evaluating volcanic provinces as markers of continental geometry and mantle organization.
Open Questions
How much information about pre-Atlantic continental configuration remains preserved within CAMP-related structures?