Publication Information

{'id': 'https://openalex.org/W4210776599', 'doi': 'https://doi.org/10.18654/1000-0569/2020.09.01', 'title': 'Partial melting of subduction zones', 'display_name': 'Partial melting of subduction zones', 'publication_year': 2020, 'publication_date': '2020-01-01', 'ids': {'openalex': 'https://openalex.org/W4210776599', 'doi': 'https://doi.org/10.18654/1000-0569/2020.09.01'}, 'language': 'en', 'primary_location': {'is_oa': False, 'landing_page_url': 'https://doi.org/10.18654/1000-0569/2020.09.01', 'pdf_url': None, 'source': {'id': 'https://openalex.org/S158389693', 'display_name': 'Acta Petrologica Sinica', 'issn_l': '1000-0569', 'issn': ['1000-0569', '2095-8927'], 'is_oa': False, 'is_in_doaj': False, 'is_core': False, 'host_organization': 'https://openalex.org/P4310319982', 'host_organization_name': 'Science Press', 'host_organization_lineage': ['https://openalex.org/P4310319982'], 'host_organization_lineage_names': ['Science Press'], 'type': 'journal'}, 'license': None, 'license_id': 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'display_name': 'Xin Dong', 'orcid': 'https://orcid.org/0000-0002-8649-7104'}, 'institutions': [], 'countries': [], 'is_corresponding': False, 'raw_author_name': 'DONG Xin', 'raw_affiliation_strings': [], 'affiliations': []}, {'author_position': 'last', 'author': {'id': 'https://openalex.org/A5110547956', 'display_name': 'Zuolin Tian', 'orcid': None}, 'institutions': [], 'countries': [], 'is_corresponding': False, 'raw_author_name': 'TIAN ZuoLin', 'raw_affiliation_strings': [], 'affiliations': []}], 'institution_assertions': [], 'countries_distinct_count': 0, 'institutions_distinct_count': 0, 'corresponding_author_ids': [], 'corresponding_institution_ids': [], 'apc_list': None, 'apc_paid': None, 'fwci': 1.13, 'has_fulltext': False, 'cited_by_count': 11, 'citation_normalized_percentile': {'value': 0.758209, 'is_in_top_1_percent': False, 'is_in_top_10_percent': False}, 'cited_by_percentile_year': {'min': 87, 'max': 88}, 'biblio': {'volume': '36', 'issue': '9', 'first_page': '2589', 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'https://openalex.org/W58593406', 'https://openalex.org/W805928198', 'https://openalex.org/W961367837'], 'related_works': ['https://openalex.org/W4387425782', 'https://openalex.org/W4205560967', 'https://openalex.org/W2732461858', 'https://openalex.org/W2392717387', 'https://openalex.org/W2378079839', 'https://openalex.org/W2359620602', 'https://openalex.org/W2205740334', 'https://openalex.org/W2121912022', 'https://openalex.org/W2044596835', 'https://openalex.org/W2044551345'], 'abstract_inverted_index': {'俯冲带是地幔对流环的下沉翼,是地球内部的重要物理与化学系统。俯冲带具有比周围地幔更低的温度,因此,一般认为俯冲板片并不会发生部分熔融,而是脱水导致上覆地幔楔发生部分熔融。但是,也有研究认为,在水化的洋壳俯冲过程中可以发生部分熔融。特别是在下列情况下,俯冲洋壳的部分熔融是俯冲带岩浆作用的重要方式。年轻的大洋岩石圈发生低角度缓慢俯冲时,洋壳物质可以发生饱和水或脱水熔融,基性岩部分熔融形成埃达克岩。太古代的俯冲带很可能具有与年轻大洋岩石圈俯冲带类似的热结构,俯冲的洋壳板片部分熔融可以形成英云闪长岩-奥长花岗岩-花岗闪长岩。平俯冲大洋高原中的基性岩可以发生部分熔融产生埃达克岩。扩张洋中脊俯冲可以导致板片窗边缘的洋壳部分熔融形成埃达克岩。与俯冲洋壳相比,俯冲的大陆地壳具有很低的水含量,较难发生部分熔融,但在超高压变质陆壳岩石的折返过程中可以经历广泛的脱水熔融。超高压变质岩在地幔深部熔融形成的熔体与地幔相互作用是碰撞造山带富钾岩浆岩的可能成因机制。碰撞造山带的加厚下地壳可经历长期的高温与高压变质和脱水熔融,形成S型花岗岩和埃达克质岩石。;Subduction': [0], 'zones': [1, 20, 133], 'are': [2], 'descending': [3], 'limbs': [4], 'of': [5, 16, 49, 60, 90, 98, 110, 125, 139, 149, 159, 165, 181, 187, 193, 209, 257, 272, 293], 'mantle': [6, 56, 63, 236, 251], 'convection': [7], 'cells,': [8], 'and': [9, 13, 28, 39, 54, 107, 122, 144, 249, 279, 282, 286, 296], 'the': [10, 25, 50, 61, 75, 84, 102, 116, 120, 126, 140, 146, 150, 157, 169, 175, 185, 191, 198, 203, 224, 232, 235, 241, 245, 250, 258, 265, 273, 291], 'major': [11], 'physical': [12], 'chemical': [14], 'system': [15], "Earth's": [17], 'interior.': [18], 'Subduction': [19], 'have': [21, 134], 'lower': [22, 270], 'temperature': [23], 'than': [24], 'adjacent': [26], 'mantle,': [27], 'therefore': [29, 145], 'it': [30], 'is': [31, 94, 252], 'proposed': [32], 'that': [33, 74], 'subducted': [34, 51, 91, 111, 151, 171, 204, 211], 'materials': [35, 113], 'including': [36], 'oceanic': [37, 52, 77, 92, 112, 128, 142, 153, 172, 182, 205], 'crust': [38, 41, 53, 78, 154, 183, 271], 'continental': [40, 212], 'do': [42], 'not': [43], 'undergo': [44], 'partial': [45, 58, 88, 147, 163, 179, 207, 284], 'melting,': [46, 285], 'whereas': [47], 'dehydration': [48, 108, 229], 'underlying': [55], 'causes': [57], 'melting': [59, 89, 109, 148, 164, 180, 208, 230], 'overriding': [62], 'wedge': [64], 'to': [65, 137, 202, 218, 237], 'generate': [66, 115], 'arc': [67, 99], 'magmatic': [68, 262], 'rocks.': [69, 177, 200, 298], 'However,': [70, 223], 'some': [71], 'studies': [72], 'concluded': [73], 'hydrated': [76], 'could': [79], 'be': [80, 215], 'partly': [81], 'molten': [82], 'during': [83, 119, 190, 231], 'subduction.': [85], 'In': [86], 'particular,': [87], 'slabs': [93], 'probably': [95], 'main': [96], 'mechanism': [97, 256], 'magmatism': [100], 'in': [101, 156, 168, 264, 287, 290], 'following': [103], 'circumstances.': [104], 'The': [105, 130, 162, 178, 268], 'water-saturated': [106], 'can': [114], 'adakitic': [117, 176, 199, 297], 'rocks': [118, 167, 226, 248, 263], 'shallow': [121], 'slow': [123], 'subduction': [124, 132, 192], 'younger': [127, 141], 'lithosphere.': [129], 'Archean': [131, 152], 'similar': [135], 'features': [136], 'those': [138], 'lithosphere,': [143], 'resulted': [155, 289], 'formation': [158, 255, 292], 'tonalite-trondhjemite-granodiorite': [160], '(TTG).': [161], 'mafic': [166], 'shallowly': [170], 'plateau': [173], 'generated': [174], 'near': [184], 'margins': [186], 'slab': [188], 'window': [189], 'spreading': [194], 'mid-oceanic': [195], 'ridge': [196], 'produced': [197], 'Contrary': [201], 'crust,': [206], 'deeply': [210], 'crusts': [213], 'should': [214], 'rare': [216], 'due': [217], 'very': [219], 'low': [220], 'water': [221], 'content.': [222], 'ultrahigh-pressure': [225, 246], 'underwent': [227], 'intensive': [228], 'exhumation': [233], 'from': [234, 244], 'crust.': [238], 'Interaction': [239], 'between': [240], 'melt': [242], 'derived': [243], 'metamorphic': [247], 'a': [253], 'potential': [254], 'potassic': [259], 'or': [260], 'ultrapotassic': [261], 'collisional': [266, 274], 'orogens.': [267], 'thickened': [269], 'orogens': [275], 'experienced': [276], 'prolonged': [277], 'high-temperature': [278], 'high-pressure': [280], 'metamorphism': [281], 'associated': [283], 'turn': [288], 'S-type': [294], 'granitoids': [295]}, 'cited_by_api_url': 'https://api.openalex.org/works?filter=cites:W4210776599', 'counts_by_year': [{'year': 2024, 'cited_by_count': 3}, {'year': 2023, 'cited_by_count': 1}, {'year': 2022, 'cited_by_count': 4}, {'year': 2021, 'cited_by_count': 3}], 'updated_date': '2025-01-05T03:36:18.576332', 'created_date': '2022-02-08'}