Researchers have discovered a 400-mile-long chain of extinct, fossilized volcanoes buried deep below South China. The volcanoes formed when two tectonic plates collided during the breakup of the supercontinent Rodinia hundreds of millions of years ago, the scientists reported in a new study. The ancient volcanoes extend the region of past volcanism in this area by several hundred miles and may have affected Earth’s climate.
About 800 million years ago, during the early Neoproterozoic era, South China sat at the northwestern margin of Rodinia. Shifting plate tectonics caused this area to break off into what is now the Yangtze Block plate, pushing it toward the China Ocean plate. As the two plates collided, the denser oceanic crust sank beneath the more buoyant continental crust and slid deep into Earth — a process known as subduction.
As oceanic crust subducts, it heats up and releases water, which generates magma. The magma rises to the surface, creating a long, narrow chain of volcanoes that follow a curved line above the subduction zone. This is known as a volcanic arc.
Volcanism and mountain building in arc systems create new crust and modify the existing crust. Therefore, researchers study ancient volcanic arcs to understand how crust formed on early Earth.
Geologists previously discovered remnants of an extinct volcanic arc along the edge of the Yangtze Block dating back to the early Neoproterozoic. In the new study, published June 30 in the Journal of Geophysical Research: Solid Earth, Zhidong Gu, a senior engineer at PetroChina, Junyong Li, a researcher at Nanjing University, and colleagues tested whether these arc volcanoes extended further inland.
Fossil mountains can be difficult to find because they’re gradually worn down by wind and water and buried beneath layers of sediment. Today, several kilometers of sedimentary rocks blanket the interior of the Yangtze Block, forming the Sichuan Basin.
Gu and Li’s team used an airborne magnetic sensor to “see” the crust beneath these sedimentary rocks. Different rock types contain different magnetic minerals, so geophysicists use magnetic signals to map underground rock formations.
They found a strip of iron-rich rock with a stronger-than-average magnetic field located about 4 miles (6 kilometers) beneath the surface. It formed an approximately 430-mile-long (700 km), 30-mile-wide (50 km) belt stretching from…
Click Here to Read the Full Original Article at Latest from Live Science…