| dc.contributor.author |
Truong, Quang Hai |
|
| dc.date.accessioned |
2011-04-15T03:10:41Z |
|
| dc.date.available |
2011-04-15T03:10:41Z |
|
| dc.date.issued |
2007 |
|
| dc.identifier.citation |
VNU. JOURNAL OF SCIENCE, Earth sciences, T.xxIII, N01, 2007 |
vi |
| dc.identifier.issn |
0866-8612 |
|
| dc.identifier.uri |
http://hdl.handle.net/123456789/177 |
|
| dc.description |
VNU. JOURNAL OF SCIENCE, Earth sciences, T.xxIII, N01, 2007 |
vi |
| dc.description.abstract |
The Voi Mep massif of the Truong Son range, having the highest peak in the
Quang Tri area (1739m), is composed of granite and granodiorite intrusive rocks in Ben
Giang-Que Son complex. This massif is fairly isometric with characteristic landforms
comprising: remnants of old pediment surfaces, mountain slopes and valleys with steep
profiles. The massif area has a regular altitudinal differentiation manifested in the formation
of two climatic belts: tropical humid climatic belt, subtropical humid climatic belt; two
altitudinal soil belts: red yellow soil belt and red yellow humus soil belt; four altitudinal
vegetation cover types: evergreen broadleaf closed forest, mixed broadleaf/needleleaf
forest, needleleaf forest and association of Arundinaria sat. The combination and interaction
of natural components led to the formation of two altitudinal landscape belts: mountain foot
tropical landscape belt and medium montane subtropical landscape belt. |
vi |
| dc.language.iso |
en |
vi |
| dc.publisher |
ĐHQGHN |
vi |
| dc.subject |
Voi Mep massif |
vi |
| dc.subject |
Núi Voi Mép |
vi |
| dc.subject |
Quang Tri |
vi |
| dc.subject |
Quảng Trị |
vi |
| dc.subject |
Đặc điểm địa hình |
vi |
| dc.title |
Characteristics of the Voi Mep massif’s altitudinal belt differentiation |
vi |
| dc.type |
Article |
vi |