3D Density Model for the Lithosphere of Alxa Block based on Gravity Inversion using Adaptive Inversion Grid Refinement in Spherical Coordinates

1 Inctroduction The study of the earth's gravitational field is an important part of the explanation of the law of evolution and the distribution of materials on the earth.Gravity satellite is a new space exploration technology rising in the 21st century,which can provide global-scale gravity measurement data,and scientists have carried out extensive research using gravity satellite data.Gravity inversion is commonly used to describe the density structure of the crust and the mantle,providing insights into geological evolution and geodynamic processes.

Carbon emission reduction:Contribution of photovoltaic power and practice in China

As a clean and renewable form of energy,photovoltaic(PV)power generation converts solar energy into electrical energy,reducing the consumption of fossil fuels and significantly lowering greenhouse gas emissions.Amidst the global transition towards cleaner forms of energy,countries all around the world are vigorously developing PV technology.

Tectonic Evolution and Lithospheric Structure of the Beishan Orogen:Insights from Magnetotelluric Studies

The Beishan orogen,located in the central segment of the Tianshan–Solonker suture within the southern Central Asian Orogenic Belt(CAOB),is crucial for understanding the accretionary processes and continental growth in Central Asia.This orogen developed through the episodic amalgamation and accretion of continental margin arcs,island arcs,ophiolites,and accretionary wedges,undergoing a complex process of accretion and evolution.Since the Phanerozoic,the Beishan orogen has experienced multiple phases of magmatic and collision events.The intricate distribution of magmatic arc rocks has obscured the complete basement traces,and the spatial superposition of multiple magmatic arc phases has complicated the study of its evolutionary history.

The Electrical Structure and Geodynamic Significance in the Alxa Block

1 Introduction The Alxa region is situated at the intersection of the Tarim Plate and the North China Plate,serving as a critical juncture between the southern boundary of the Central Asian Orogenic Belt(CAOB)and the Alxa Block(Song et al.,2020)(Fig.1).This region connects the Tianshan and Beishan orogens to the west with the Solonker suture to the east,offering a unique vantage point for examining the evolution of the Paleo-Asian Ocean.

Electrical Resistivity Structures of the Beishan Block,NW China,and Tectonic Implications

The Central Asian Orogenic Belt(CAOB)is a giant orogenic belt located between the Siberian Plate,the Tarim Plate,and the North China Plate,which records the longterm and complex geologic evolution of the Paleo-Asian Ocean from the Early Neoproterozoic(ca.1000 Ma)to the Late Paleoproterozoic(ca.250 Ma)process.The Beishan Block is located in the middle and southern edge of the Central Asian orogenic belt,at the intersection of the Tarim plate,the Siberian Plate and the Kazakhstan Plate.