logo

What is controlling plate motions over the minutes to decades timescale?

Sector: Telecommunications • Location: Germany

Source: EU Funding & Tenders Portal

Project
Ongoing

Tectonic ground observations from Global Navigation Satellite Systems (GNSS) increasingly show that plate motions are non-steady. In some instances, these non-steady motions have been suspected as precursory motions to large earthquakes. However, the full spectral behaviour of transient plate motions, across minutes to decades, and kilometres to continental distances, is not well understood. Her

Project Information FAQ

Project Information

4 Q
The project “What is controlling plate motions over the minutes to decades timescale?” is an infrastructure initiative in the Telecommunications sector, located in Germany. Taiyo aggregates data on it from EU Funding & Tenders Portal.

Want to explore the full details? View the full report

Participants

Sponsoring Agency

Obfuscated Data

Company

Obfuscated Data

Status

Original status

ongoing

Taiyo status

Obfuscated Data

Taiyo last update

00-00-0000

Available timestamps

00-00-0000

Available timestamp type

Obfuscated Data

Contact

Contact name

Obfuscated Data

Phone

0000000000

Email

ObfuscatedData@email.com

Address

Obfuscated Data, Obfuscated data, obfuscated data, Obfuscated data

Description

Description

Tectonic ground observations from Global Navigation Satellite Systems (GNSS) increasingly show that plate motions are non-steady. In some instances, these non-steady motions have been suspected as precursory motions to large earthquakes. However, the full spectral behaviour of transient plate motions, across minutes to decades, and kilometres to continental distances, is not well understood. Here, I propose a multi-pronged approach to study how faults and plates worldwide are moving in response to the geodynamical (interior) and geophysical fluid loading/tidal (exterior) boundary conditions. The major questions to address are: How transient is tectonic deformation over the minutes to decades timescale? What are the physical processes controlling the transient plate motions? To what extent are transient plate motions indicative of earthquake imminence? We will reveal the extent of non-linear tectonic motions by developing GNSS processing algorithms and applying these to data from the thousands of tectonic GNSS stations worldwide. With machine learning, numerical modelling, and laboratory experimentation, we will determine to what extent faults are modulated by variable regional tectonics and loading. We will develop kinematic and laboratory modelling strategies to better understand transient tectonic boundary conditions such as transient slab-pull at subduction zones. While analysis will span continental and global scales, we will also investigate the kinematics of faults and fault networks with dense GNSS observations at a higher resolution, using GNSS and seismic data from north-central Chile as well as from laboratory-scale analog modelling to track fault failure in unprecedented detail. In Greece, a world-class example of a seismically hazardous zone of fault-network complexity, we will set up a world’s first low-cost tectonic GNSS network to understand how microplate motions interact with the larger wavelength tectonic boundary conditions of the region.

Original sub-sector

Obfuscated

Original Currency

USD

Original budget

000000000000000

Procurement method

Obfuscated Data

Budget

000000000000000

Location

Region

Obfuscated

Country

Obfuscated

State

Obfuscated Data

County

Obfuscated

Location

Obfuscated Data, Obfuscated data, obfuscated data, Obfuscated data

Source

Source reliability

High

Data quality score

100%

Source

Obfuscated Data

URL

obfuscated_data,obfuscateddata.com

More Details

Project Type

Obfuscated Data

Article Published Date

Obfuscated Data