[HTML][HTML] Layered intrusions: Fundamentals, novel observations and concepts, and controversial issues
Layered intrusions are fossilized natural laboratories that historically have constrained many
fundamental principles of igneous petrology. Layered intrusions are typically stratiform …
fundamental principles of igneous petrology. Layered intrusions are typically stratiform …
The life cycle of large igneous provinces
Extremely voluminous magmatic systems known as large igneous provinces (LIPs)
punctuate Earth's history, and the gases they release plausibly link large-scale geodynamic …
punctuate Earth's history, and the gases they release plausibly link large-scale geodynamic …
High-precision geochronology confirms voluminous magmatism before, during, and after Earth's most severe extinction
SD Burgess, SA Bowring - Science advances, 2015 - science.org
The end-Permian mass extinction was the most severe in the Phanerozoic, extinguishing
more than 90% of marine and 75% of terrestrial species in a maximum of 61±48 ky. Because …
more than 90% of marine and 75% of terrestrial species in a maximum of 61±48 ky. Because …
Large igneous provinces and silicic large igneous provinces: Progress in our understanding over the last 25 years
Large igneous provinces are exceptional intraplate igneous events throughout Earth's
history. Their significance and potential global impact are related to the total volume of …
history. Their significance and potential global impact are related to the total volume of …
The largest volcanic eruptions on Earth
Large igneous provinces (LIPs) are sites of the most frequently recurring, largest volume
basaltic and silicic eruptions in Earth history. These large-volume (> 1000km3 dense rock …
basaltic and silicic eruptions in Earth history. These large-volume (> 1000km3 dense rock …
[PDF][PDF] Does large igneous province volcanism always perturb the mercury cycle? Comparing the records of Oceanic Anoxic Event 2 and the end-Cretaceous to other …
Mercury (Hg) is increasingly being used as a sedimentary tracer of Large Igneous Province
(LIP) volcanism, and supports hypotheses of a coincidence between the formation of several …
(LIP) volcanism, and supports hypotheses of a coincidence between the formation of several …
Source to sink: a review of three decades of progress in the understanding of volcaniclastic processes, deposits, and hazards
V Manville, K Németh, K Kano - Sedimentary Geology, 2009 - Elsevier
Volcaniclastic sediments, broadly defined as clastic deposits derived from the transport,
deposition and/or redeposition of the products of volcanic activity, have long been a …
deposition and/or redeposition of the products of volcanic activity, have long been a …
Determination of rapid Deccan eruptions across the Cretaceous‐Tertiary boundary using paleomagnetic secular variation: Results from a 1200‐m‐thick section in the …
Flow‐by‐flow reanalysis of paleomagnetic directions in two sections of the Mahabaleshwar
escarpment, coupled with analysis of intertrappean alteration levels shows that volcanism …
escarpment, coupled with analysis of intertrappean alteration levels shows that volcanism …
Episodic warming of early Mars by punctuated volcanism
The widespread evidence for liquid water on the surface of early Mars is difficult to reconcile
with a dimmer early Sun. Many geomorphological features suggestive of aqueous activity …
with a dimmer early Sun. Many geomorphological features suggestive of aqueous activity …
[HTML][HTML] Tracing volcanic emissions from the Central Atlantic Magmatic Province in the sedimentary record
The end-Triassic mass extinction (ETME) is thought to have been caused by voluminous,
pulsed volcanic activity of the Central Atlantic Magmatic Province (CAMP). Over the last …
pulsed volcanic activity of the Central Atlantic Magmatic Province (CAMP). Over the last …