DOCSLIB.ORG
Explore
Sign Up
Log In
Upload
Search
Home
» Tags
» Izanagi Plate
Izanagi Plate
Origin and Time Evolution of Subduction Polarity Reversal
Late Cretaceous and Paleogene Tectonic Evolution of the North Pacific Ocean
A Plate Model for Jurassic to Recent Intraplate Volcanism in the Pacific Ocean Basin
Origin and Time Evolution of Subduction Polarity Reversal from Plate Kinematics of Southeast Asia
Global Plate Boundary Evolution and Kinematics Since the Late Paleozoic
Convergence of Tectonic Reconstructions and Mantle Convection Models for Significant Fluctuations in Seafloor Spreading Nicolas Coltice, Maria Seton, Tobias Rolf, R.D
A Global Isochron Chart
A Plate Reconstruction Model of the NW Pacific Region Since 100 Ma
The Cretaceous and Cenozoic Tectonic Evolution of Southeast Asia
Reconstructing Jurassic‐Cretaceous Intra‐Oceanic Subduction Evolution
Revised History of Izanagi-Pacific Ridge Subduction
Pacific Plate Slab Pull and Intraplate Deformation in the Early Cenozoic
On the Enigmatic Birth of the Pacific Plate Within the Panthalassa Ocean Lydian M
Mid-Mantle Heterogeneities Associated with Izanagi Plate: Implications for Regional Mantle Viscosity ∗ Juan Li A, , David A
List of Plate Ids to Accompany Seton Et. Al. Global Model 000 Hotspots
Speculations on Cretaceous Tectonic History of the Northwest Pacific and a Tectonic Origin for the Hawaii Hotspot
Izanagi-Pacific Ridge Subduction Revealed by a 56 to 46 Ma
Recognition of a Middle–Late Jurassic Arc-Related Porphyry Copper Belt
Top View
Download Preprint
Late Paleozoic-Mesozoic Tectonic Evolution of SW Japan: a Review -Reappraisal of the Accretionary Orogeny and Revalidation of the Collisional Model Jacques Charvet
Subduction Duration and Slab
A Global-Scale Plate Reorganization Event at 105−100Ma
Hierarchical Self-Organization of Tectonic Plates
Ridge Subduction Sparked Reorganization of the Pacific Plate
The Cretaceous and Cenozoic Tectonic Evolution of Southeast Asia
Izanagi-Pacific Ridge Subduction Revealed by a 56 to 46 Ma Magmatic Gap Along the Northeast Asian Margin
An Unrecognized Major Collision of the Okhotomorsk Block with East Asia During the Late Cretaceous, Constraints on the Plate Reorganization of the Northwest Pacific
Plate-Tectonic Reconstructions Predict Part of the Hawaiian Hotspot Track to Be Preserved in the Bering Sea
33. Paleolatitudes and Tectonic Reconstructions of the Oldest Portion of the Pacific Plate: a Comparative Study1