<?xml version="1.0" encoding="UTF-8"?>
<feed xmlns:dc="http://purl.org/dc/elements/1.1/" xmlns="http://www.w3.org/2005/Atom">
<title>Vol. 23, No.3</title>
<link href="http://tainguyenso.vnu.edu.vn/jspui/handle/123456789/55" rel="alternate"/>
<subtitle/>
<id>http://tainguyenso.vnu.edu.vn/jspui/handle/123456789/55</id>
<updated>2026-05-19T23:39:24Z</updated>
<dc:date>2026-05-19T23:39:24Z</dc:date>
<entry>
<title>Building a GIS database for ecotourism development in Ba Vi District, Ha Tay Province, Vietnam</title>
<link href="http://tainguyenso.vnu.edu.vn/jspui/handle/123456789/1523" rel="alternate"/>
<author>
<name>Nguyen, Dinh Minh</name>
</author>
<id>http://tainguyenso.vnu.edu.vn/jspui/handle/123456789/1523</id>
<updated>2011-04-21T03:44:35Z</updated>
<published>2007-01-01T00:00:00Z</published>
<summary type="text">Building a GIS database for ecotourism development in Ba Vi District, Ha Tay Province, Vietnam
Nguyen, Dinh Minh
Ecotourism is a concept and a fast growing segment of the tourism industry worldwide.&#13;
It plays an increasingly important role in the socio‐economic development of many districts and&#13;
provinces in Vietnam. Therefore, it needs to be well planned and managed with the aid of spatial&#13;
information technologies such as Remote Sensing (RS), Geographic Information System (GIS) and&#13;
Global Positioning System (GPS). This paper presents the results of building a GIS database for&#13;
ecotourism development in Ba Vi, a large legendary mountainous district of Ha Tay Province based&#13;
on field and desk investigations. The created database consists of spatial and attributive data files&#13;
related to natural and cultural resources in Ba Vi stored in a standard format of ArcView GIS that&#13;
can and should be effectively retrieved, analyzed and updated to generate useful information in the&#13;
form of maps, tables and charts to support ecotourism planning and management activities in the&#13;
district for sustainable development.
VNU Journal of Science, Earth Sciences. Vol. 23 (2007), No. 3, P. 146‐151
</summary>
<dc:date>2007-01-01T00:00:00Z</dc:date>
</entry>
<entry>
<title>On some significant unconformities in the Paleozoic and Mesozoic stratigraphy of North Viet Nam Mesozoic stratigraphy of North Viet Nam</title>
<link href="http://tainguyenso.vnu.edu.vn/jspui/handle/123456789/1513" rel="alternate"/>
<author>
<name>Tong, Dzuy Thanh</name>
</author>
<id>http://tainguyenso.vnu.edu.vn/jspui/handle/123456789/1513</id>
<updated>2011-04-21T03:40:35Z</updated>
<published>2007-01-01T00:00:00Z</published>
<summary type="text">On some significant unconformities in the Paleozoic and Mesozoic stratigraphy of North Viet Nam Mesozoic stratigraphy of North Viet Nam
Tong, Dzuy Thanh
A lot of unconformities and stratigraphic gaps have been discovered in the Paleozoic and&#13;
Mesozoic stratigraphy of Bac Bo region (North Viet Nam), but their role in the regional geology&#13;
was not accessed yet in detail. This paper is the first attempt to describe the most significant&#13;
unconformities and stratigraphic gaps and discussing their role in regional geology. The most&#13;
important is the angular unconformity of Norian‐Rhaetian formations upon various formations of&#13;
different formations; it marked the change tectonic regime of the region resulting from the indosian&#13;
orogeny in Viet Nam and in Southeast Asia in common. The gap of Lower Devonian red beds&#13;
formations (Si Ka Formation, Song Cau Group) upon Lower Paleozoic formations (Upper Cambrian ‐&#13;
Than Sa Formation, Lower Ordovician ‐ Lutxia and Na Mo formations) is a regional unconformity,&#13;
which had been taken place in the epicaledonian terranne of South China and North East of Viet&#13;
Nam. The gap between the Da Mai Formation and the Dong Dang Formation was a result of a crust&#13;
rising, but was not through the orogeny activity, although after this gap the structural plan was&#13;
more differentiated. Other unconformities and stratigraphic gaps seems to be local unconformities,&#13;
for instance, the one of the Tan Lap Formation (D2g‐D3 fr tl) upon the Ban Pap Formation (D1p‐D3 fr bp)&#13;
and the unconformity between the Sinh Vinh (O3‐S sv) and the Ben Khe (ε‐O1 bk) formations.
VNU Journal of Science, Earth Sciences. Vol. 23 (2007), No. 3, P. 137‐146
</summary>
<dc:date>2007-01-01T00:00:00Z</dc:date>
</entry>
</feed>
