@curator

9 months ago

Article

Earth's evolving geodynamic regime recorded by titanium isotopes - Nature

Rating: 0.0

Likes: 1

Library: 1

Earth's evolving geodynamic regime recorded by titanium isotopes - Nature

Earth's mantle has a two-layered structure, with the upper and lower mantle domains separated by a seismic discontinuity at about 660 km (refs. 1,2). The extent of mass transfer between these mantle domains throughout Earth's history is, however, poorly understood. Continental crust extraction results in Ti-stable isotopic fractionation, producing isotopically light melting residues3–7. Mantle recycling of these components can impart Ti isotope variability that is trackable in deep time.

Rating: 0.0

Likes: 1

Library: 1

Rate This Post

Rate The Educational Value

Rate The Ease of Understanding and Presentation

Interesting or Boring? Rate the Entertainment Value

Earth's evolving geodynamic regime recorded by titanium isotopes - Nature

Rate This Post

Related Topics

Comments

Media:

My Account:

Boostlane:

Select a Category

Topics Trending Today

Recommended Media

Boostlane Reward System

Unlocking the Power of Knowledge
for Humanity's Progress

Quick Links

Select a Locale

Unlocking the Power of Knowledge
for Humanity's Progress

Earth's evolving geodynamic regime recorded by titanium isotopes - Nature

Rate This Post

Related Topics

Comments

Media:

My Account:

Boostlane:

Select a Category

Topics Trending Today

Recommended Media

Boostlane Reward System

Unlocking the Power of Knowledge for Humanity's Progress

Quick Links

Select a Locale

Unlocking the Power of Knowledge for Humanity's Progress

Unlocking the Power of Knowledge
for Humanity's Progress

Unlocking the Power of Knowledge
for Humanity's Progress