In the aftermath of the September 11th events,the trend ofAmerican relations with Arab nations has become the importantfactor that influences the evolution of international pattern.Particular-ly,the changes of America...In the aftermath of the September 11th events,the trend ofAmerican relations with Arab nations has become the importantfactor that influences the evolution of international pattern.Particular-ly,the changes of American-Saudi relations attract worldwide atten-tion.This article tries to make a brief analysis and comment on the fea-展开更多
In the issue of January, 2002, the magazine "Relation Between Both Sides of the Taiwan Straits" published by the Association of the Relation Between the Both Sides of the Taiwan Straits, a signed essay was c...In the issue of January, 2002, the magazine "Relation Between Both Sides of the Taiwan Straits" published by the Association of the Relation Between the Both Sides of the Taiwan Straits, a signed essay was carried out, stating that the development of the relation between the both sides last year, anticipates the trends of such relation in the future.展开更多
Nowadays,multilateral consultative mechanism is gradually becoming a mainstream approach in the contemporary international system.As one of the most important international collective player,the European Union(EU) has...Nowadays,multilateral consultative mechanism is gradually becoming a mainstream approach in the contemporary international system.As one of the most important international collective player,the European Union(EU) has been engaging in multilateral cooperation and consultation since its inception.It has also been promoting a plural world through advocacy and action.The EU and the Latin America/Caribbean(LAC) Countries summits are considered a stability mechanism for promoting bi-regional dialogues.Nevertheless,after 10 years of bi-regional strategic partnership construction,the EU and LAC relations are currently experiencing a difficult phase,suggesting it is time to reform.The purpose of this paper is to analyze the advantages as well as the challenges to EU-LAC relations from the perspective of bi-regional summits,and to assess the short-term trend of their relations in the near展开更多
Since 2014, the development of the China-India relationship has followed a trend of starting high and ending low. The China-India relationship warmed up rapidly in the first two years, which nevertheless failed to bri...Since 2014, the development of the China-India relationship has followed a trend of starting high and ending low. The China-India relationship warmed up rapidly in the first two years, which nevertheless failed to bring about a substantial breakthrough in their bilateral relations, as India's strategic doubts about China and their differences of interests on numerous issues still pose difficulties.展开更多
Three major types of Ordovician intrusive-related gold-copper deposits are recognized in central-west New South Wales, Australia: porphyry, skarn and high sulphidation epithermal deposits. These deposits are mainly di...Three major types of Ordovician intrusive-related gold-copper deposits are recognized in central-west New South Wales, Australia: porphyry, skarn and high sulphidation epithermal deposits. These deposits are mainly distributed within two Ordovician volcano-intrusive belts of the Lachlan Fold Belt: the Orange-Wellington Belt and the Parkes-Narromine Belt. Available isotopic age data suggest that mineralization of the three types of deposits is essentially coeval with the Ordovician intrusive rocks (480-430 Ma).Porphyry gold-copper deposits can be further divided into two groups. The first group is associated with monzonite showing shoshonitic features, represented by Cadia and Goonumbla. The second group is associated with diorite and dacite, including the Copper Hill and Cargo gold-copper deposits. Gold skarn is associated with Late Ordovician (430-439 Ma) monzonitic intrusive complexes in the Junction Reefs area (Sheahan-Grants, Frenchmans, and Cor-nishmens), Endeavour 6, 7 and 44, Big and Little Cadia. The epithermal gold deposits with high sulphidation including Gidginbung (Temora) and Peak Hill mainly occur within Ordovician andesite and volcaniclastic rocks, and are associated with advanced argillic alteration. Available isotopic age data indicate that both alteration and mineralization of the porphyry, skarn and epithermal gold-copper deposits are broadly coeval with the Late Ordovician shoshonitic magmatism, which is thought to result from the melting of sub-continental lithosphere caused by Palaeozoic subduction events.The Ordovician intrusive-related gold-copper deposits are restricted to two longitudinal parallel volcano-intrusive belts, rarely extending outside them. Diagonal intra-belt trends of mineralization are common, particularly at the intersections of longitudinal and transverse (oblique) fault/fracture zones based on the authors' review of available geological data. The locations of these gold-copper deposits are obviously influenced by transverse (oblique) fault/fracture zones that are oriented northwest, eastwest and northeast. The conjunctions of these fault/fractures zones are thought to be zones of structural weakness, and appear to be the favourable locus for the Ordovician intrusive-related gold-copper deposits. Differences in structural patterns, intrusive, wall rock types, and depths of ore formation may contribute to the differences among the deposits.展开更多
文摘In the aftermath of the September 11th events,the trend ofAmerican relations with Arab nations has become the importantfactor that influences the evolution of international pattern.Particular-ly,the changes of American-Saudi relations attract worldwide atten-tion.This article tries to make a brief analysis and comment on the fea-
文摘In the issue of January, 2002, the magazine "Relation Between Both Sides of the Taiwan Straits" published by the Association of the Relation Between the Both Sides of the Taiwan Straits, a signed essay was carried out, stating that the development of the relation between the both sides last year, anticipates the trends of such relation in the future.
文摘Nowadays,multilateral consultative mechanism is gradually becoming a mainstream approach in the contemporary international system.As one of the most important international collective player,the European Union(EU) has been engaging in multilateral cooperation and consultation since its inception.It has also been promoting a plural world through advocacy and action.The EU and the Latin America/Caribbean(LAC) Countries summits are considered a stability mechanism for promoting bi-regional dialogues.Nevertheless,after 10 years of bi-regional strategic partnership construction,the EU and LAC relations are currently experiencing a difficult phase,suggesting it is time to reform.The purpose of this paper is to analyze the advantages as well as the challenges to EU-LAC relations from the perspective of bi-regional summits,and to assess the short-term trend of their relations in the near
文摘Since 2014, the development of the China-India relationship has followed a trend of starting high and ending low. The China-India relationship warmed up rapidly in the first two years, which nevertheless failed to bring about a substantial breakthrough in their bilateral relations, as India's strategic doubts about China and their differences of interests on numerous issues still pose difficulties.
文摘Three major types of Ordovician intrusive-related gold-copper deposits are recognized in central-west New South Wales, Australia: porphyry, skarn and high sulphidation epithermal deposits. These deposits are mainly distributed within two Ordovician volcano-intrusive belts of the Lachlan Fold Belt: the Orange-Wellington Belt and the Parkes-Narromine Belt. Available isotopic age data suggest that mineralization of the three types of deposits is essentially coeval with the Ordovician intrusive rocks (480-430 Ma).Porphyry gold-copper deposits can be further divided into two groups. The first group is associated with monzonite showing shoshonitic features, represented by Cadia and Goonumbla. The second group is associated with diorite and dacite, including the Copper Hill and Cargo gold-copper deposits. Gold skarn is associated with Late Ordovician (430-439 Ma) monzonitic intrusive complexes in the Junction Reefs area (Sheahan-Grants, Frenchmans, and Cor-nishmens), Endeavour 6, 7 and 44, Big and Little Cadia. The epithermal gold deposits with high sulphidation including Gidginbung (Temora) and Peak Hill mainly occur within Ordovician andesite and volcaniclastic rocks, and are associated with advanced argillic alteration. Available isotopic age data indicate that both alteration and mineralization of the porphyry, skarn and epithermal gold-copper deposits are broadly coeval with the Late Ordovician shoshonitic magmatism, which is thought to result from the melting of sub-continental lithosphere caused by Palaeozoic subduction events.The Ordovician intrusive-related gold-copper deposits are restricted to two longitudinal parallel volcano-intrusive belts, rarely extending outside them. Diagonal intra-belt trends of mineralization are common, particularly at the intersections of longitudinal and transverse (oblique) fault/fracture zones based on the authors' review of available geological data. The locations of these gold-copper deposits are obviously influenced by transverse (oblique) fault/fracture zones that are oriented northwest, eastwest and northeast. The conjunctions of these fault/fractures zones are thought to be zones of structural weakness, and appear to be the favourable locus for the Ordovician intrusive-related gold-copper deposits. Differences in structural patterns, intrusive, wall rock types, and depths of ore formation may contribute to the differences among the deposits.
