Researchers found evidence that the Aleutian Islands' subduction beneath the North American Plate occurred at least 56 million years ago, significantly earlier than previously thought. This discovery has implications for understanding tectonic and climatic processes that shaped the Earth's history.
Researchers have refined the timing and duration of Ocean Anoxic Event 1a, an extreme environmental disruption that caused significant extinction among plankton. The study determined OAE 1a lasted for just over 1.1 million years, providing valuable insights into Earth's climate and ocean system.
Researchers have discovered living microbes in a 2-billion-year-old rock sample from the Bushveld Igneous Complex in South Africa. The team used advanced imaging techniques to confirm the presence of indigenous microorganisms, shedding light on the early evolution of life on Earth and the potential for similar organisms to exist on Mars.
Researchers propose that Mars' early thick atmosphere could have been locked up in the planet's clay surface due to slow chain reactions between rocks and gases. The clay is estimated to hold up to 80% of the initial, early atmosphere, potentially recovered and converted into propellant for future missions.
A Rice-led team studied massif-type anorthosites to understand their formation, revealing they likely originated from melting of subducted oceanic crust beneath convergent continental margins. The research provides new insights into Earth's thermal and tectonic evolution and chronicles the physical evolution of our planet.
The Perseverance rover has collected and remotely determined the original orientations of most bedrock samples to date. This breakthrough will help scientists answer key questions about Mars' past, including its magnetic field, water flow, and tectonic processes.
The rover has discovered primary igneous rocks and hydrated magnesium sulfate, hinting at the presence of ancient life on Mars. The mission aims to retrieve samples that may answer the question about whether we are alone in the universe.
Researchers identified seven exotic igneous clasts in Chang'e-5 samples, providing critical information about the Moon's lithological diversity and regolith gardening process. The findings indicate that there are still unknown geological units on the moon, which may aid future lunar exploration missions.
Researchers used molybdenum isotopes to study the interaction between subducting slabs and mantles. They found systematic differences in the isotopic composition of rocks from different depths, indicating distinct metasomatism processes. This helps understand the structure of subduction zones.
A new study suggests that massive volcanic eruptions were the primary cause of mass extinctions, including the one that wiped out the dinosaurs. The research found a strong temporal connection between flood basalt eruptions and significant climatic events.
The Perseverance rover has collected the first Martian rock samples that could be returned to Earth, shedding light on whether Mars ever hosted life. The rock samples come from the Jezero crater floor, where scientists believe a watery past may have supported life.
The Perseverance rover collected igneous cumulate rocks from four sites on the floor of Jezero Crater, providing evidence of aqueous alteration. These rocks will help scientists determine when Mars' climate was conducive to lakes and rivers, addressing major questions about the planet's history.
A team of researchers identified an unusual belt of igneous rocks stretching over 2,000 miles from Canada to Mexico, defying expectations of volcanic activity. The rock formation, dated to 80-50 million years ago, originated deep underground and lacks evidence of volcanoes.
Research by University of Liverpool reveals strange magnetic behaviour in South Atlantic region dated back eight to 11 million years ago. The study suggests that today's South Atlantic Anomaly is not a new phenomenon and may be linked to features of the Earth's interior.
A study suggests that Triassic igneous rocks in Brazil caused the release of light carbon isotopes, which may have contributed to the end-Triassic extinction. The findings imply a significant impact on the Earth's carbon cycle during this period.
Researchers found two dramatic decreases in thorium-uranium ratios at 2.35 and 0.75 billion years ago, consistent with established dates for the Great Oxidation and Neoproterozoic Oxygenation Events.
A new UCL-led study has pinpointed the exact locations of two quarries in Wales that supplied the bluestones to Stonehenge. The discovery reveals how the stones were quarried and transported, challenging a popular theory about their transportation method.
Researchers caution that relying solely on zircon crystals can skew timescales for geological events, potentially millions of years. The findings have implications for understanding volcanic hazards and predicting future risks.
Scientists discovered the Midcontinent Rift evolved in three stages: a narrow crack, volcanic rock filling, and igneous rocks rising to surface. The rift's unique geology was formed by magma flowing into the developing crack and eventually creating a large igneous province.
Researchers found rich deposits of feldspar, a mineral common in granite, in an ancient Martian volcano. The discovery suggests prolonged magmatic activity on Mars, leading to the formation of granite-like rocks, challenging previous assumptions about Martian geology.
Researchers analyzing Martian rocks using Curiosity rover's chemical instruments found a pyramid-shaped volcanic rock called a mugearite, similar to those on Earth. The discovery suggests the presence of water deep below Mars' surface, a crucial ingredient for life.
Researchers discovered that heavier isotopes separate from lighter isotopes as magma cools down due to their greater mass and momentum. This separation, called fractionation, can provide insights into the formation of igneous rocks.
A new study by the University of Chicago reveals that Greenland's ancient rocks are sedimentary and not igneous, providing evidence for biological activity 3.85 billion years ago. The findings support the search for early life on Earth and open up new possibilities for research.