The role of plume-ridge decoupling on rapid plate motion
Ben Mather , Maria Seton, Simon Williams, Jo Whittaker, Rebecca Carey, Maëlis Arnould, Nicolas Coltice, Bob Duncan Iceland Ridge Plate motion driven by: Slab pull at subduction …
ben-mather
Ben Mather
•
Jun 27, 2023 9:00 AM — 10:00 AM
•
1 min read
Kimberlite eruptions driven by slab flux and subduction angle
Machine learning reveals that the volume and angle of subducted oceanic plates control where and when diamond-bearing kimberlite eruptions occur.
ben-mather
The role of plume-ridge decoupling on rapid plate motion and intraplate volcanism
Ben Mather , Maria Seton, Simon Williams, Jo Whittaker, Rebecca Carey, Maëlis Arnould, Nicolas Coltice, Bob Duncan LIPs repeatedly form at locations where plumes and ridges …
ben-mather
Deep time spatio-temporal data analysis using pyGPlates with PlateTectonicTools and GPlately
GPlately: a Python interface for deep-time spatio-temporal data analysis using pyGPlates, simplifying plate tectonic reconstructions.
ben-mather
The isotopic origin of Lord Howe Island reveals secondary mantle plume twinning in the Tasman Sea
First radiogenic isotope data from Lord Howe Island lavas reveal a secondary mantle plume twin in the Tasman Sea with a distinct deep mantle source.
angus-rogers
Accelerating spatio -temporal data analysis using pyGPlates
The GIS interface of GPlates is cumbersome for spatio -temporal data analysis PyGPlates is an open-source Python library to visualise and edit plate tectonic reconstructions …
ben-mather
Anomalously High Heat Flow Regions Beneath the Transantarctic Mountains and Wilkes Subglacial Basin in East Antarctica Inferred From Curie Depth
Curie depth estimates from airborne magnetic data reveal anomalously high geothermal heat flow beneath the Transantarctic Mountains and Wilkes Subglacial Basin.
maximilian-lowe
Geodynamic modelling update
OVERVIEW OF INTRAPLATE VOLCANISM Glass House Mountains, QLD Last Eruption: 24 million years ago
ben-mather
Iron isotope systematics during igneous differentiation in lavas from Kīlauea and Mauna Loa, Hawai'i
Iron isotope and hafnium data from Kīlauea and Mauna Loa lavas reveal how igneous differentiation and mantle source heterogeneity shape Hawaiian volcanism.
saskia-ruttor
Unravelling the origins of volcanism along Eastern Australia and the Tasman Sea
Mantle plumes are buoyant upwellings rising from the Earth’s core-mantle boundary to its surface, generating hotspot chains that track the direction of plate motion. Eastern …
ben-mather