Seawater silica cycling and chert formation at the Neoproterozoic–Cambrian transition: Insights from δ30Si and Ge/Si systematics of hydrothermal cherts from the Bohemian Massif-Reference-Cited by-同舟云学术

Seawater silica cycling and chert formation at the Neoproterozoic–Cambrian transition: Insights from δ30Si and Ge/Si systematics of hydrothermal cherts from the Bohemian Massif

Published:2023-09 Issue: Volume:634 Page:121598
ISSN:0009-2541
Container-title:Chemical Geology
language:en
Short-container-title:Chemical Geology

Author:

Ackerman Lukáš,Poitrasson Franck,Magna Tomáš,Polák Ladislav,Ďurišová Jana

Publisher

Elsevier BV

Subject

Geochemistry and Petrology,Geology

Reference105 articles.

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3. Carbon, oxygen, and strontium isotopic fingerprint in Neoproterozoic to early Cambrian limestones in an active margin setting: a record of local environment or global changes?;Ackerman;Precambrian Res.,2022

4. The significance of cherts as markers of Ocean Plate Stratigraphy and paleoenvironmental conditions: New insights from the Neoproterozoic–Cambrian Blovice accretionary wedge, Bohemian Massif;Ackerman;Geosci. Front.,2023

5. Silicon isotopes in ∼3.8 Ga West Greenland rocks as clues to the Eoarchaean supracrustal Si cycle;André;Earth Planet. Sci. Lett.,2006

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1. Geochemistry of cherts from the northern Jiangxi region, South China: Implication for paleoenvironment;Journal of Palaeogeography;2024-07

2. Formation of Ediacaran stromatolitic cherts through a combination of biogenic and abiotic processes: New insights from the Bohemian Massif;Precambrian Research;2024-06