J 2023

THEORY OF CONTINENTAL DRIFT - CAUSES OF THE MOTION. OUTLINE OF THE THEORY

KALENDA, Pavel, Libor NEUMANN, Ivo WANDROL, Vaclav PROCHAZKA, Lubor OSTRIHANSKY et. al.

Basic information

Original name

THEORY OF CONTINENTAL DRIFT - CAUSES OF THE MOTION. OUTLINE OF THE THEORY

Authors

KALENDA, Pavel, Libor NEUMANN, Ivo WANDROL (203 Czech Republic, belonging to the institution), Vaclav PROCHAZKA and Lubor OSTRIHANSKY

Edition

GEODYNAMICS, 2023, 1992-142X

Other information

Language

English

Type of outcome

Článek v odborném periodiku

Field of Study

10700 1.7 Other natural sciences

Country of publisher

Ukraine

Confidentiality degree

není předmětem státního či obchodního tajemství

References:

RIV identification code

RIV/47813059:19630/23:A0000327

Organization unit

Institute of physics in Opava

UT WoS

001146762300005

Keywords in English

Continental drift;motion of plates;mechanism;solar energy accumulation

Tags

Tags

International impact, Reviewed
Změněno: 29/2/2024 07:36, Mgr. Pavlína Jalůvková

Abstract

V originále

The theory of mantle convection currents as the cause of lithospheric plate movements has several major problems, including the absence of an adequate energy source. As shown in our previous contribution, an unbiased interpretation of geochemical data does not support the assumptions of a significant amount of radionuclides in the lower mantle or even in the core. It is our assertion that solar radiation is the primary energy source in the lithosphere. This energy is converted into mechanical energy via thermoelastic waves, even in depths with minimal temperature fluctuations. This has been confirmed by various methods of continuous stress measurement. The periodic and quasiperiodic thermoelastic reversible deformations, such as the circadian and annual cycles (including tidal periods), can also cause irreversible deformations due to the ratcheting mechanism. The 2D model showed that the strength limit is exceeded in 0.3 % of all diurnal cycles during the year. As a consequence, continents tend to extend while the oceanic lithosphere is pushed and overthrusted between continents. The middle-ocean ridges, similar to continental rifts, are filled by ascending magma which is one example of the ratcheting mechanism. The final plate movements are determined by the distribution of major continents and the overall westward drift of the lithosphere, which is slower for deep-rooted plates like the Indian one. Large asteroid impacts are important triggers (and possibly significant energy sources) of discrete events, like the formation of hotspots and large igneous provinces.