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| 1 | Characteristics and potential analysis of Madagascar hydrocarbon-bearing basins显示文摘Madagascar becomes a large isolated island after its dislocation from East Africa at its western part during the opening of the Mozambique Channel and its separation from India at its eastern part during the opening of the basin of the Mascarene. From a stratigraphic point of view, Karroo of Madagascar shares substantial similarities with the stratigraphic strata of East Africa.While oil companies have taken a liking to the basins of East Africa, they also turn to the basins in the western part of Madagascar especially after the discovery of large oil fields at Tsimiroro and Bemolanga. According to the study of their geological history, the basins of Madagascar contain huge hydrocarbon potential. The western basins, which is more developed than the east coast of the island, have been the subject of many in-depth studies by numerous researchers. The cross-referencing of bibliographic data with geological studies, and knowledge of hydrocarbon formation and maturation stages, carried out in this study served to determine the nature of source rocks, reservoir rocks, bedrock and eventual trapping system of hydrocarbons in Madagascar. This study identified the properties of Madagascar source rocks, reservoir rocks, bedrock and the final oil and gas trap system by cross-referencing the literature and geological research, oil and gas formation and maturity stages, and shows that Madagascar has considerable hydrocarbon potential. | Da-tian Wu Johanne Iomimalala Ramaniraka Feng-ming Xu Jian-bo Shao Yong-heng Zhou Yuan-dong Zhao Bruno Ralison | 2019 | China Geology2019，2，1： | 2 |
| 2 | Post-collisional magmatism in the central East African orogen: The Maevarano suite of north Madagascm显示文摘 | Goodenough K M Thomas R J De Waele B Key R M Schofield D I Bauer W Tucker R D Kafahatelo J M Rabrimanana M Ralison A V Randriamananjma T | 2010 | Lithos2010，116，12： | 1 |
| 3 | Angraecoid orchids and hawkmoths in central Madagascar: specialized pollination systems and genelist foragers 显示文摘 | Nilsson L A Jonsson L Ralison L Randrianjohany E | 1987 | Biotropica1987，19，： | 1 |
| 4 | Oxidation of orthorhombic Ti2 AlNb alloys in the temperaturer ange 500-1000 ℃ in air显示文摘 | Ralison A R Dettenwanger F D Schütze M S | | 0，，20： | 1 |
| 5 | Carbon biogeochemistry in the Betsiboka estuary (northwestern Madagascar) 显示文摘 | Ralison O H Borges A V Dehairs F | 2008 | Organic Geochemistry2008，39，： | 1 |
| 6 | Structure and metamorphism of the granitic basement around Antananarivo: A key to the Pan-African history of central Madagascar and its Gondwana connections 显示文摘 | N6d61ec A Ralison B Bouchez J L | 2000 | Tectonics2000，19，： | 1 |
| 7 | Carbon biogeochemistry of the Betsiboka estuary(north-western Madagascar)显示文摘 | Ralison O H Borges A V Dehairs F | 2008 | Organic Geochemistry2008，39，12： | 1 |
| 8 | Oxidation of orthorhombic Ti2 A1Nb alloys at 800~C in air显示文摘 | Ralison A Dettenwanger F Sehiitze M | 2000 | Materials and Corrosion2000，，5： | 1 |
| 9 | Oxidation of ortho-rliomhic Ti, AINh alloys at 800 °C in air显示文摘 | Ralison A Dettenvvanger F Sohiitze M | | Materials andCorrosion0，51，5： | 1 |
| 10 | Oxidation of orthorhombic Ti2AINb alloys at 800C in air显示文摘 | Ralison A Dettenwanger F Schiitze M | 2000 | Materials anti Corrosion2000，51，5： | 1 |
| 11 | Oxidation of orthorhombic Ti2AlNb alloys at 800 ℃ in air显示文摘 | RALISON A DETTEMWAMGER F SCHüTZE M | 2000 | Materials and Corrosion2000，51，5： | 1 |
| 12 | Oxidation of orthorhombic Ti2AlNb alloys in the temperature range 550-1000 degrees C in air显示文摘 | RALISON A DETTENWANGER F SCHUZE M | 2003 | Mater High Temp2003，20，： | 1 |
| 13 | Oxidation of orthorhombic Ti2AlNb alloys at 800 ℃ in air显示文摘 | RALISON A DETTENWANGER F SCHUZE M | 2000 | Mater Corros2000，51，： | 1 |
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