2019
DOI: 10.1016/j.jseaes.2018.09.010
|View full text |Cite
|
Sign up to set email alerts
|

Structure and evolution of the Ban Pong Basin, Chiang Mai Province, Thailand

Help me understand this report

Search citation statements

Order By: Relevance

Paper Sections

Select...
1
1
1

Citation Types

0
3
0

Year Published

2019
2019
2024
2024

Publication Types

Select...
6

Relationship

0
6

Authors

Journals

citations
Cited by 6 publications
(3 citation statements)
references
References 27 publications
0
3
0
Order By: Relevance
“…In addition to the mountainous landscape of Chiang Mai's westernmost region, the province boasts a variety of other diverse terrains i.e., dense forests, valleys, and rolling hills. This province is the northern region's largest intermontane basin, characterized by its location within the Chiang Mai Basin (Mankhemthong, 2019). The area is notable for its complex geological processes and formations.…”
Section: Study Areamentioning
confidence: 99%
See 1 more Smart Citation
“…In addition to the mountainous landscape of Chiang Mai's westernmost region, the province boasts a variety of other diverse terrains i.e., dense forests, valleys, and rolling hills. This province is the northern region's largest intermontane basin, characterized by its location within the Chiang Mai Basin (Mankhemthong, 2019). The area is notable for its complex geological processes and formations.…”
Section: Study Areamentioning
confidence: 99%
“…To the best of our knowledge, previously, there has been no research related to the STK ensemble modelling of landslide susceptibility in our experimental area. The study will be conducted in Chiang Mai Province, Thailand, which is known for its intermontane basin topography and is highly susceptible to landslides, particularly in hilly areas (Wattananikorn et al, 1995;Mankhemthong, 2019). Almost 10% of the region's population lives in landslide-prone areas.…”
Section: Introductionmentioning
confidence: 99%
“…The Doi Inthanon and Doi Suthep are two metamorphic core complexes in northern Thailand ductilely deformed in the Oligocene followed by post-kinematic intrusions at 27 Ma (Dunning et al, 1995). The Chiang Mai Basin formed by the end of the Oligocene and available AFT ages indicate an exhumation and cooling to upper crustal levels between ~24 Ma and 18 Ma (Mankhemthong et al, 2018;Morley, 2009;Upton, 1999). Upton et al (1997), conducted a thermal modelling for one sample with sufficient track lengths of the Doi Inthanon complex, and estimated cooling rates between 8.5 °C / Ma and 25 °C / Ma corresponding to a denudation of 550-3500 m/Ma which is in accordance with our cooling rates through the APAZ in Khanom.…”
Section: A Northward Migration Of the Chain Of Eventsmentioning
confidence: 99%