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SUPPLEMENTARY INFORMATION AND DATA for: Cambrian foreland phosphogenesis in the Khuvsgul Basin of Mongolia; Anttila et al., 2025.

Mendeley Data2026-04-09 收录

沉积磷矿化作用

前陆盆地

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SUPPLEMENTARY INFORMATION AND DATA for: Cambrian foreland phosphogenesis in the Khuvsgul Basin of Mongolia; Anttila et al., 2025.

应用场景：

地质学

前陆盆地

Supplementary material A (Kangjiagou section sandstone petrographic composition data)

DataCite Commons2024-02-13 更新60

Data for: Migration model of hydrocarbons in the slope of the superimposed foreland basin: A case study from the South Junggar, NW China

油气运移模拟

前陆盆地

Migration model of hydrocarbons in the slope of the superimposed foreland basin: A case study from the South Junggar Basin, NW China

NIAID Data Ecosystem40

Provenance of detrital zircons in the Late Triassic Sichuan foreland basin: constraints on the evolution of the Qinling Orogen and Longmen Shan thrust-fold belt in central China

碎屑锆石物源分析

前陆盆地

In this article, we present in situ U–Pb and Lu–Hf isotope data for Upper Triassic detritus in the Sichuan region of northwestern South China, which was a foreland basin during the Late Triassic. The

NIAID Data Ecosystem40

Table1_Early late triassic retro-foreland basin in response to flat subduction of the Paleo-Tethyan oceanic plate, SE tibet.DOCX

前陆盆地

古特提斯洋俯冲机制

Syn-subduction basins bear significant implications to understand tectonic evolution of any fossil subduction zone. The late Paleozoic to early Mesozoic (Paleo-Tethyan) tectonics of the eastern and so

NIAID Data Ecosystem50

Original seismic data in "Growth of the Tian Shan drives migration of the conglomerate-sandstone transition in the southern Junggar foreland basin"

地震地质构造

前陆盆地

Here is the original seismic data presented in the manuscript entitled "Growth of the Tian Shan drives migration of the conglomerate-sandstone transition in the southern Junggar foreland basin"(# 2021

NIAID Data Ecosystem40

SUPPLEMENTARY INFORMATION AND DATA for: Cambrian foreland phosphogenesis in the Khuvsgul Basin of Mongolia; Anttila et al., 2025.

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