Structural data - Agly massif

Name: Structural data - Agly massif
Creator: Laboratoire Chrono-environnement
Published: 2023-02-07T14:23:30+08:00

DataCite Commons2025-12-11 更新2025-04-17 收录

构造地质学

岩石变形分析

数据链接：

https://search-data.ubfc.fr/FR-18008901306731-2021-11-25_Structural-data-Agly-massif.html 数据链接链接失效反馈

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资源简介：

Structural database of foliations, schistosities and lineations of variscan ductile structures of the Agly massif.

提供机构：

Laboratoire Chrono-environnement

创建时间：

2023-02-07

Ti-in quartz thermobarometry for Bhutan quartz mylonites

地质学

构造地质学

Abstract: Ti-in-quartz thermobarometry (TitaniQ) is based on the pressure and temperature (P-T) dependence of the solubility of titanium in quartz (Huang & Audetat, 2012; Kawasaki & Osanai, 2008; Osta

DataONE2021-01-18 更新60

Tectonic escape of a crustal fragment during the closure of the Rheic Ocean: U–Pb detrital zircon data from the Late Palaeozoic Pulo do Lobo and South Portuguese zones, southern Iberia

地质学

构造地质学

The Pulo do Lobo Zone, which crops out immediately north of the allochthonous South Portuguese Zone in southern Iberia, is classically interpreted as a polydeformed accretionary complex developed alon

DataCite Commons2020-09-04 更新30

Beaumont numbers and associated values of several mountain belts on Earth

构造地质学

地球动力学

This file contains the data shown in table 1 in the Article: Tectonics or Surface Processes during orogenesis - the Beaumont number: II. Application to orogens on Earth. Variable definitions:NAndes ar

Zenodo2023-11-17 更新20

Mid-Miocene North–south Trending Dikes in the Aduo Basin of Northeastern Tibet: New Constraints on the Timing of Plateau Uplift

岩石地球化学

构造地质学

The research data used in the paper " Mid-Miocene North–south Trending Dikes in the Aduo Basin of Northeastern Tibet: New Constraints on the Timing of Plateau Uplift " submitted to GR

Figshare2023-05-17 更新40

Coupling X-ray microtomography imaging and acoustic emission monitoring to unravel laboratory earthquakes: The KORE apparatus

实验室地震模拟

岩石变形分析

Earthquakes initiate at 5-15 km depth and cannot be observed directly in situ. Therefore, laboratory experiments were developed in the past 50 years to reproduce and study laboratory earthquakes to un

ESRF Portal2024-01-01 更新30

Structural data - Agly massif

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