Identification of delta types critical for accurate prediction of future change in deltas
收藏NIAID Data Ecosystem2026-03-13 收录
官方服务:
资源简介:
it includes Data tables (.doc), and simulation package (.zip) and medias of Run 19 and Run 30
应用场景:
创建时间:
2022-05-20
相关数据集
Advances and perspectives in numerical modeling for geodynamics
The dynamic processes in Earth’s deep interior are key driving forces behind geological events and play a fundamental role in Earth’s evolution. Their mechanisms and surface responses have been centra
中国科学数据2026-02-27 更新10
Elevation projections for the Mekong delta (Vietnam) under sedimentation strategies, subsidence, compaction, and sea-level rise
Modelled elevation projections for the Mekong delta (Vietnam) to 2050 under scenarios of fluvial sedimentation, organic accumulation, anthropogenic-accelerated subsidence, natural compaction, and glob
Zenodo2021-11-05 更新00
Dataset and Software: Heat Transfer in Pyroclastic Density Current - Ice Interactions: Insights from Experimental and Numerical Simulations
This repository contains experiment data and executable MATLAB codes for the research article 'Heat Transfer in Pyroclastic Density Current - Ice Interactions: Insights from Experimental and Numerical
NIAID Data Ecosystem00
DataSheet1_Computational simulation of the ore-forming processes associated with the Sanshandao-Haiyu gold belt, Jiaodong Peninsula, eastern China: implications for the duration of ore formation.doc
The Sanshandao-Haiyu gold belt, Jiaodong Peninsula, Eastern China accounts for more than 1,400 t gold resources, which is always recognized as a coupled result of structural deformation, pore-fluid fl
NIAID Data Ecosystem00
Buoyancy versus local stress field control on the velocity of magma propagation: insight from analog and numerical modelling, Supporting Data
Experimental data and numerical codes used in the manuscript "Buoyancy versus local stress field control on the velocity of magma propagation: insight from analog and numerical modelling" by V. Pinel,
Zenodo2021-12-20 更新00



