Jump to main content
US EPA
United States Environmental Protection Agency
Search
Search
Main menu
Environmental Topics
Laws & Regulations
About EPA
Health & Environmental Research Online (HERO)
Contact Us
Print
Feedback
Export to File
Search:
This record has one attached file:
Add More Files
Attach File(s):
Display Name for File*:
Save
Citation
Tags
HERO ID
7069330
Reference Type
Journal Article
Title
Refined chronostratigraphy of the late Mesozoic terrestrial strata in South China and its tectono-stratigraphic evolution
Author(s)
Li, X; Zhang, C; Li, Y; Wang, Yin; Liu, L; ,
Year
2019
Is Peer Reviewed?
Yes
Journal
Gondwana Research
ISSN:
1342-937X
Publisher
ELSEVIER SCIENCE BV
Location
AMSTERDAM
Page Numbers
143-167
DOI
10.1016/j.gr.2018.09.006
Web of Science Id
WOS:000468246900009
Abstract
The late Mesozoic terrestrial strata in numerous basins in S (South) China provide important sedimentary archives to understand the tectonic evolution of S China and East Asia. However, establishing regional stratigraphic framework within a basin and precisely correlating strata among basins remain challenging clue to limited chronological constraints. In this study, we report zircon U-Pb ages of 21 samples and a compilation of 132 reliable age data from 15 type sections of the volcanic -sedimentary basins in S China. The synthesized geochronology allows us to establish a refined chronostratigraphy for the late Mesozoic terrestrial strata. New calibrated results indicate that most of the lithostratigraphic units are diachronic, laterally stacking, and/or interfingering. Six stacking styles are classified for the relationship of lithostratigraphic units. Analysis of the refined chronostratigraphy and the strata! stacking styles, together with lithological composition, reveals three episodes of tectono-stratigraphic evolution. Episode I (-145-125 Ma) is characterized by intense volcanism, as evidenced by widespread occurrence of volcanic strata and (137-120 Ma) A-type granites. and was probably related to the rollback of the subducting Paleo-Pacific plate; The strata deposited during Episode II (-125-100 Ma) are composed of variegated sediments associated with/without volcanic intercalations in sedimentary faulted-depression basins, indicating the waning of volcanism and tectonism attributed to the ending of the Izanagi/Kula plate subduction: In Episode Ill (<-100 Ma), red strata occurred along the NE -SW sinistral strike-slip faulting or failed rifting in small basins, which probably resulted from the drastic directional change of the Paleo-Pacific plate subduction from NW to SN. (C) 2019 International Association for Gondwana Research. Published by Elsevier B.V. All rights reserved.
Home
Learn about HERO
Using HERO
Search HERO
Projects in HERO
Risk Assessment
Transparency & Integrity