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1
Intro
2
Introduction to Southeast Asia
3
The Scale of SE Asia (Indonesia and Malaysia)
4
Tectonic Assembly of SE Asia
5
Continental Blocks
6
Arc Volcanism
7
Tectonic Plate Convergence
8
Issues with Reconstructions
9
History of Sedimentation
10
Mountainous Rivers
11
Estimated Sediment Yields
12
Example from the Salin Sub-basin, Myanmar
13
Map of the Cenozoic Basins
14
Data Locations SE Asia
15
Dating of Basement Rocks
16
Field Studies
17
Light Mineral Database
18
Gazzi-Dickinson Models
19
An Example from Borneo Borneo QmFLt
20
Volcanic Quartz
21
Heavy Mineral Database
22
Supported by Raman Spectroscopy
23
Heavy Minerals - Myanmar
24
Heavy Minerals for Palaeoenvironment
25
U-Pb Zircon Ages
26
Foraminifera Database
27
Using Forams to Date Arc Collision
28
Palaeogeographies - Eocene
29
Conclusions
Description:
Explore the complexities of reconstructing palaeogeographies in tropical climates through a comprehensive 58-minute lecture focusing on Southeast Asia. Delve into the challenges posed by poor exposure and heavily weathered outcrops in regions like Indonesia and Malaysia. Learn how combining light minerals, heavy minerals, and detrital grain age analyses can fill gaps in geological understanding. Examine the tectonic assembly of SE Asia, including continental blocks, arc volcanism, and plate convergence. Investigate sedimentation history, mountainous rivers, and estimated sediment yields, with a specific example from the Salin Sub-basin in Myanmar. Study various databases and methodologies, including light and heavy mineral analyses, Gazzi-Dickinson models, U-Pb zircon dating, and foraminiferal studies. Discover how these diverse data sets contribute to reconstructing Eocene palaeogeographies and resolving complex tectonic histories in tropical regions.

How Big Data Can Resolve Regional Palaeogeographies in Tropical Climates

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