Surge-tectonic evolution of southeastern Asia: a geohydrodynamics approach

Meyerhoff, A. A.

doi:10.1016/0743-9547(95)00028-3

Cited by 8 publications

(4 citation statements)

References 430 publications

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“…L'existence d'un point triple tectonique rend la synthèse de l'histoire géologique de cette région incomplète et sujette à débats (Hutchison, 1989;Meyerhoff, 1995;Wilson & Moss, 1999), mais des données fondamentales permettent de dresser une trame. L'évolution physiographique de l'Indonésie est marquée par deux phénomènes géologiques majeurs : la tectonique des plaques et le volcanisme qui lui est associé régionalement.…”

Section: Discussion: Tentative D'explication Embryonnaire Sur Ce Qui unclassified

Unité et diversité préhistorique entre Java et Sumatra

Forestier¹,

Simanjuntak²,

Détroit³

et al. 2010

arch

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Prehistoric Unity and Diversity of Java and Sumatra The comparison of the archaeological records of Java and Sumatra allows to present a preliminary assessment defining future researches to be implemented in order to address major questions such as the origin of the “ Austronesians”. The geographical fates of both islands are different for modern humans and obviously played an important role, shared or separated, in the history and prehistory of Indonesia. From 20 000 to 5 000 BP, Java is marked by a technical heterogeneity in produced stone tools. In the meantime, Sumatra shows more homogenous technical choices, with a unifacial pebble shaping which still belongs to the Hoabinhian tradition. Recent palaeoanthropological data from Java indicate a large variability in funerary practices as well. Different types of burials, partial cremations and other mortuary practices are documented diachronically and synchronically. Consistent data related to funerary practices are still needed regarding Sumatra.

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Section: Discussion: Tentative D'explication Embryonnaire Sur Ce Qui unclassified

Unité et diversité préhistorique entre Java et Sumatra

Forestier¹,

Simanjuntak²,

Détroit³

et al. 2010

arch

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show abstract

“…无论持上述何种认识, 东亚陆缘大地构造演化必然涉及这些可能与古太平洋板块俯冲关联的缝合线的讨论, 基于这些认识, 对其东亚陆缘响应也提出过很多观点, 例如: 地体构造、转换断层俯冲 [31,34,35] 、涌动构造 [77] 、板片窗 [78,79] 、挤出构造 [3,56] 、俯冲堵塞 [71,80] 等种种构造模型和演化历程, 但一致认为该陆缘印 [51] . 中国华南或南岭山地 [20] 和朝鲜半岛北部 [81] [85,86] (图4), 最终, 东亚陆缘标志成熟岛弧出现的大套钙碱性岩浆岩带出现在燕山期, 此时才出现高大的安第斯型海岸山脉.…”

Section: 露有串珠状基性-超基性岩体因而可能只是一条类unclassified

“…,207] , 支持洋中脊垂直欧亚板块东部陆缘的俯冲消减模式(图11). 板片窗构造主要出现在125~110 Ma左右 [79,207] (图11), 形成了中国东部长江中下游独特的成矿和埃达克岩等岩浆作用 [79] , 以及日本和吕宋岛等的110 Ma的岩浆岩异常 -埃达克岩 [77,78,209] , 这似乎也表现在日本125~60 Ma的花岗岩类空间分布总体表现为向北西开口的"V 字形" [52] . 对照东太平洋陆缘, 按照最新板块重建成果, 库拉板块(图11(c))只是太平洋板块在70~20 Ma 期间位于阿拉斯加南部和加拿大东部海域的古板块 [31] , 其相关洋中脊俯冲导致在阿留申群岛上出现了 [31] 的重建, 55 Ma之后才可能发生洋中脊俯冲, 依泽奈崎-太平洋板块之间的洋中脊平行东亚陆缘, 其状况可能类似环文林等人 [210] 的大陆边缘构造复原图, 不可能出现典型的板片窗, 即使出现, 也应晚于55 Ma 时间, 而这之后华南又不存在埃达克岩分布 [149] .…”

Section: 台湾海峡金门岛、马祖岛、长乐岛的花岗片麻岩时代为109~92unclassified

Mesozoic plate subduction in West Pacific and tectono-magmatic response in the East Asian ocean-continent connection zone

Suo

et al. 2018

Chin. Sci. Bull.

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“…The equatorial Atlantic region of the Mid-Atlantic Ridge includes Blocks E, F, and G (Figs. 5 and 6) and has long been recognized as a region of considerable structural complexity that contains old rocks (Meyerhoff andMeyerhoff, 1974a, 1974b;Honnorez et LII., 1975;Udinetsev and Agapova, 1991;Meyerhoff et al, 1992a). It is also a region of comparatively low heat flow ( 4 5 mW/m') along the mid-ocean ridge system, where heat-flow values in the crestal zone normally are very high (>60 mW/m?…”

Section: Pertinent Geological Data From the North Atlantic Basinmentioning

confidence: 99%

Tectonic Fabric of the Atlantic Ocean Floor: Speculation vs. Reality

Smoot

Meyerhoff²

1995

Journal of Petroleum Geology

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the late) A. A. MeyerhofP"Almost all published charts of the world's ocean floors have been drawn deliberately to reflect the predictions of the plate-tectonics hypothesis. For example, the Atlantic Ocean floor is unvaryingly shown to be dominated by CI sinuous, north-south mid-ocean ridge, flanked on either side by abyssalplains, cleft at its crest by a rijit valley, und offset at more-or-less regular 40to 60-km intervals by east-west-striking fracture cones. However. it is now clear that as new, detailed, bathymetric surveys are being completed, this oversimplified portrayal of the Atlantic Basin is largely wrong. Thousands of bathymetric features present, many of them major, are wholly unexplained by plate tectonics. Others, predicted by plate tectonics, are totally absent. We show, on the basis of specific examples based on real data from the North Atlantic Ocean, that the real bathymetiy and the real tectonic fabricare very differentfrom the bathymetry and tectonic fabric portrayed (but rarely documented) in plate-tectonics publications. A new hypothesis is needed to explain the origin of the real bathymetry and tectonic fabric of the deep oceans. Such CI hypothesis could very wellprovide clues forfuture petroleum and other mineral exploration along the continental margins.

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Surge-tectonic evolution of southeastern Asia: a geohydrodynamics approach

Cited by 8 publications

References 430 publications

Unité et diversité préhistorique entre Java et Sumatra

Unité et diversité préhistorique entre Java et Sumatra

Mesozoic plate subduction in West Pacific and tectono-magmatic response in the East Asian ocean-continent connection zone

Tectonic Fabric of the Atlantic Ocean Floor: Speculation vs. Reality

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