| Calibrating the terminations of Cryogenian global glaciations |
30 |
| Appalachian-style multi-terrane Wilson cycle model for the assembly of South China |
27 |
| Marine redox fluctuation as a potential trigger for the Cambrian explosion |
27 |
| Arid Central Asia saw mid-Holocene drought |
26 |
| How to recognize crescentic bedforms formed by supercritical turbidity currents in the geologic record: Insights from active submarine channels |
25 |
| Ocean euxinia and climate change double whammy drove the Late Ordovician mass extinction |
23 |
| Depressurization and boiling of a single magmatic fluid as a mechanism for tin-tungsten deposit formation |
23 |
| Congruent Permian-Triassic delta U-238 records at Panthalassic and Tethyan sites: Confirmation of global-oceanic anoxia and validation of the U-isotope paleoredox proxy |
21 |
| Mercury enrichments and the Frasnian-Famennian biotic crisis: A volcanic trigger proved? |
21 |
| Timing of the Arabia-Eurasia continental collision-Evidence from detrital zircon U-Pb geochronology of the Red Bed Series strata of the northwest Zagros hinterland, Kurdistan region of Iraq |
21 |
| New U-Pb dates show a Paleogene origin for the modern Asian biodiversity hot spots |
19 |
| Desiccation cracks provide evidence of lake drying on Mars, Sutton Island member, Murray formation, Gale Crater |
18 |
| Strontium and carbon isotopic evidence for decoupling of pCO(2) from continental weathering at the apex of the late Paleozoic glaciation |
18 |
| Absolute ages of multiple generations of brittle structures by U-Pb dating of calcite |
18 |
| North Atlantic temperature and pCO(2) coupling in the early-middle Miocene |
17 |
| Precise age of Bangiomorpha pubescens dates the origin of eukaryotic photosynthesis |
17 |
| Laurentian crust in northeast Australia: Implications for the assembly of the supercontinent Nuna |
17 |
| Nano-porous pyrite and organic matter in 3.5-billion-year-old stromatolites record primordial life |
15 |
| Textural and compositional evidence for the formation of pentlandite via peritectic reaction: Implications for the distribution of highly siderophile elements |
15 |
| A 6000-km-long Neo-Tethyan arc system with coherent magmatic flare-ups and lulls in South Asia |
15 |
| Reconstructing the Anak Krakatau flank collapse that caused the December 2018 Indonesian tsunami |
15 |
| Arsenic evolution as a tool for understanding formation of pyritic gold ores |
14 |
| Late Cenozoic magmatic inflation, crustal thickening, and >2 km of surface uplift in central Tibet |
14 |
| Explosive volcanism as a key driver of the late Paleozoic ice age |
14 |
| Subduction initiation dynamics along a transform fault control trench curvature and ophiolite ages |
14 |
| Erosional surfaces in the Upper Cretaceous Castlegate Sandstone (Utah, USA): Sequence boundaries or autogenic scour from backwater hydrodynamics? |
14 |
| Discovery of vast fluvial deposits provides evidence for drawdown during the late Miocene Messinian salinity crisis |
14 |
| Mercury evidence of intense volcanic effects on land during the Permian-Triassic transition |
13 |
| Genesis of the world's largest rare earth element deposit, Bayan Obo, China: Protracted mineralization evolution over similar to 1 b.y. |
13 |
| Subsiding Sundaland |
13 |
| Cu isotopes reveal initial Cu enrichment in sources of giant porphyry deposits in a collisional setting |
13 |
| 1.6 Ga crustal thickening along the final Nuna suture |
13 |
| A new model for transformation of ferrihydrite to hematite in soils and sediments |
13 |
| A shallow origin for diamonds in ophiolitic chromitites |
13 |
| Opening of glacial Lake Agassiz's eastern outlets by the start of the Younger Dryas cold period |
13 |
| Unzipping continents and the birth of microcontinents |
13 |
| Dehydration-induced rheological heterogeneity and the deep tremor source in warm subduction zones |
13 |
| U-Pb dating of calcite cement and diagenetic history in microporous carbonate reservoirs: Case of the Urgonian Limestone, France |
13 |
| Elastic geothermobarometry: Corrections for the geometry of the host-inclusion system |
13 |
| How long can the middle crust remain partially molten during orogeny? |
12 |
| Constraining the maximum depth of brittle deformation at slow- and ultraslow-spreading ridges using microseismicity |
12 |
| Diverse biomineralizing animals in the terminal Ediacaran Period herald the Cambrian explosion |
12 |
| A positive test for the Greater Tarim Block at the heart of Rodinia: Mega-dextral suturing of supercontinent assembly |
12 |
| The pace of crustal-scale magma accretion and differentiation beneath silicic caldera volcanoes |
12 |
| Long-term in situ observations on typhoon-triggered turbidity currents in the deep sea |
11 |
| Generation of alkaline magmas in subduction zones by partial melting of melange diapirs-An experimental study |
11 |
| A mineralogical signature for Burgess Shale-type fossilization |
11 |
| Seismically anisotropic magma reservoirs underlying silicic calderas |
11 |
| The Bayan Obo (China) giant REE accumulation conundrum elucidated by intense magmatic differentiation of carbonatite |
11 |
| 3-D seismic images of an extensive igneous sill in the lower crust |
11 |
