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This boundary, called the K-T, or Cretaceous(K)-Tertiary(T) boundary, is around 65 million years ago and marks the point which dinosaurs are no longer found in the rock record.
Malay ko
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The impact of a meteorite about 65 million years ago that caused mass extinction on Earth.
well none of the ocean crust is more than 175 million years old because subduction happens. subduction is when an ocean plate moves slowly into a continent plate and then goes under it and get devoured by the mantle because its lighter than the continental crust. so the answer to your question would be around the edges of the pacific plate.
I think you are referring to the 'iridium spike' - the Yucatan impactor brought to earth a quantity of iridium that was deposited and is detectable at the K-T boundary (the Cretaceous - Tertiary boundary) wherever this is found round the planet.
This boundary, called the K-T, or Cretaceous(K)-Tertiary(T) boundary, is around 65 million years ago and marks the point which dinosaurs are no longer found in the rock record.
I t means Extending out above or beyond a surface or boundary
The temperature in kelvins at which the reaction is happening
Malay ko
An estimation is 50.106 t in the earth crust and oceans.
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it is t t is the letters
1. There is an unusually high concentration of Iridium found at the K-T boundary. Iridium loves to stick to Iron, so the Iridium that would have been on Earth originally is in the Iron core, not in the crust. Therefore, the Iridium must have been introduced by an external source; a meteorite. 2. Shocked Quartz is found at the K-T Boundary all around North America. Shocked Quartz is only produced naturally by bolide impact. Since the K-T meteorite impacted in the Mexican peninsula, it makes sense that the shocked quartz would be found only in relatively close proximity to the impact site. 3. Microtektites, which are normally found at meteorite impact sites, are found at all K-T boundary impact sites. 4. There is a massive impact crater in the Mexican peninsula. 5. In many of the K-T Boundary sections there is a fine layer of ash (disseminated Carbon) from the global wildfires that were caused. 6. There was a fern spike because other flowering plants stopped producing pollen for awhile. 7. Microdiamonds have been detected at K-T Boundary sites, but not above or below.
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The KT Boundary (also called the Cretaceous-Paleogene, or K-Pg boundary) is a boundary marking the Cretaceous-Tertiary extinction (KT extinction) event. It is usually seen as a thin band, caused by an asteroid impact that wiped out much of life at the time.
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