Do more with less: Exploring semi-supervised learning for geological image classification
Labelled datasets within geoscience can often be small, with data acquisition both costly and challenging, and their interpretation and downstream...
Deepdive Leveraging Pre-trained Deep-Learning for Deep-Sea ROV Biota Identification in the Great Barrier Reef
Understanding and preserving the deep sea ecosystems is paramount for marine conservation efforts. Automated object (deep-sea biota) classification can enable...
Pore pressure penetrometers document high overpressure near the seafloor where multiple submarine landslides have occurred on the continental slope, offshore Louisiana, Gulf of Mexico
Overpressures measured with pore pressure penetrometers during Integrated Ocean Drilling Program (IODP) Expedition 308 reach 70% and 60% of the...
Environmental precursors to rapid light carbon injection at the Palaeocene/Eocene boundary
The Palaeocene/Eocene thermal maximum — a period of intense global warming about 55 million years ago — was associated with...
Clumped Isotope Reordering and Kinetic Differences in Co-Hosted Calcite and Dolomite Minerals throughout Burial Diagenesis and Exhumation
The clumped isotope paleo-thermometer has become a valuable proxy for the burial history reconstruction of carbonate formations. To maximise the...
DIAGENESIS OF THE CENTRAL LUCONIA CARBONATE PLATFORMS: THE ROLES OF EARLY DOLOMITIZATION AND LATE HYDROTHERMAL FLUIDS IN ENHANCING DEEP RESERVOIR PROPERTIES
The Central Luconia Miocene carbonate platform represents one of the largest regions of Liquified Natural Gas (LNG) production in the...
Object detection algorithms to identify skeletal components in carbonate cores
Identification of constituent grains in carbonate rocks requires specialist experience. A carbonate sedimentologist must be able to distinguish between skeletal...
Mechanism of island dolostones formation in the Cretaceous calcitic ocean: Insights from the Mid-Pacific Guyots
Dolomite is common in carbonate successions. There is an ongoing debate about the origin of ancient massive dolostones. Recent studies...
Reconstructing the temperature and origin of CO2 mineralisation in CarbFix calcite using clumped, carbon and oxygen isotopes
In-situ CO2 mineralisation has been demonstrated as a rapid and secure mechanism of geological CO2 storage through a series of...
Mineral carbonation of peridotite fueled by magmatic degassing and melt impregnation in an oceanic transform fault
Most of the geologic CO2 entering Earth’s atmosphere and oceans is emitted along plate margins. While C-cycling at mid-ocean ridges...