The Franklin dike swarm, also called the Franklin dikes, is a Proterozoic dike swarm of the Franklin Large Igneous Province in Northern Canada. It is one of the several major magmatic events in the Canadian Shield and it was formed 723 million years ago. Areas in the Franklin have been prospected for nickel, copper, and platinum group metals.[1]
The Franklin dike swarm occupies a major part of the Franklin Large Igneous Province, which covers an area of more than 2,000,000 km2 (770,000 sq mi).[2]
^"Regional Metallogeny Large Igneous Provinces in Canada Through Time and Their Metallogenic Potential". Mineral Deposits of Canada. Geological Survey of Canada. 2008-09-25. Archived from the original on 2010-04-20. Retrieved 2009-07-19.
^Reconstructing Ancient Continents Using the Large Igneous Province Record: Implications For Mineral, Hydrocarbon, and Earth Systems
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The Franklindikeswarm, also called the Franklindikes, is a Proterozoic dikeswarm of the Franklin Large Igneous Province in Northern Canada. It is one...
A dikeswarm (American spelling) or dyke swarm (British spelling) is a large geological structure consisting of a major group of parallel, linear, or radially...
large Franklindikeswarm, which extends for more than 1,200 km (750 mi) across the Canadian Arctic Archipelago and northwestern Greenland. The Franklin Large...
than 570 Mya and traces of this breakup can still be found in the Franklindikeswarm in northern Canada and the Aldan Shield in Siberia. The Proto-Pacific...
Lakes in Northwestern Ontario where it meets with the smaller Matachewan dikeswarm. Included in the Mackenzie Large Igneous Province are the large Muskox...
gold and molybdenum deposits; and around the Franklindikeswarm in Canada. Mapping the presence of dikes allows us to understand how magma (molten rock...
significant event was the magmatism that formed the 723‑million-year-old Franklindikeswarm of Northern Canada and has been heavily mined for nickel, copper...
years ago, these units were capped with dacite associated with the Franklindikeswarms and the doming of the western Arctic. Glacial material in the Rapitan...
feeder dikeswarms associated with the Steens Basalt flow are considered to be atypical of other dikeswarm trends associated with the CRBG. These swarms, characterized...
1972). The Northwest Territories contains the Mackenzie dikeswarm, which is the largest dikeswarm known on Earth. Around 1,269-1,267 million years ago...
Igneous Province forms 1,270 million years ago. Mistassini dikeswarm and Matachewan dikeswarm form 2,500 million years ago. Blake River Megacaldera Complex...
quartz-feldspar-porphyry and quartz monzonite subvolcanic plutons and dikeswarms. They intrude through fractured and hydrothermally altered Mesozoic to...
northwest-trending dikes composed of diabase may represent extensions of the 1,250 million year old Sudbury dikeswarm. This dikeswarm is older than the...
result in the emplacement of dikeswarms, such as those that are observable across the Canadian shield, or rings of dikes around the lava tube of a volcano...
fractures serve as feeders for fault intrusions that are also known as ring dikes. Secondary volcanic vents may form above the ring fracture. As the magma...
the north. Magma intrusions of diabase rocks 765 million years ago left dikes that can be seen on the east face of Mount Moran and Middle Teton. Granite...
1910; a family-scale placer-mining operation continues today. Granitic dikeswarms cutting the shales and sandstones of the Kuskokwim Group rocks in the...
Center. Retrieved April 12, 2020. "Canal Is Opened by Wilson's Finger; Gamboa Dike Blown Away as President in Washington Presses Button". New York Times. October...
activity took place from the Paleozoic to Cenozoic with the emplacement of dikes, sills, lava flows and pyroclastic rocks. The Sverdrup Basin Magmatic Province...
threatened to break through the dikes protecting the town of Șendreni, as locals and emergency services reinforced the dikes with sandbags by the truck-full...