1824年,荷兰国王威廉一世以皇家决议的方式建立了尼德兰贸易公司(Nederlandsche Handel-Maatschappij,简称NHM)。该公司于1964年同屯特银行(Twentsche Bank)合并组成通用荷兰银行(Algemene Bank Nederland,简称ABN)。同年,阿姆斯特丹银行(Amsterdamsche Bank)同鹿特丹银行(Rotterdamsche Bank)合并组成了阿姆斯特丹与鹿特丹银行(AMRO Bank,简称AMRO银行)。最终,在1991年,通用荷兰银行同阿姆斯特丹与鹿特丹银行合并组成荷兰银行。
2007年4月23日,荷兰银行与英国巴克莱银行(Barclays Bank)宣布达成协议,巴克莱银行收购荷兰银行。[1]但這項決議於2007年10月被蘇格蘭皇家銀行(Royal Bank of Scotland)、富通銀行(Fortis Bank)、桑坦德銀行(Banco Santander)三家銀行集團,宣佈以1010億美金購併荷兰銀行的計畫所取代。其主要原因在於新的併購集團除了購併價格提高之外,其現金的支付比例由原來的79%提高到93%,因此得到持有荷兰銀行86%股份的股東支援,最後終能擊敗英國巴克萊銀行的競爭[2]。之後富通銀行所持有的股份轉賣給荷兰政府。
Clash Royale CLAN TAG #URR8PPP A coarse-grained mafic intrusive rock Gabbro Photomicrograph of a thin section of gabbro Gabbro ( / ˈ ɡ æ b r oʊ / ) is a phaneritic (coarse-grained), mafic intrusive igneous rock formed from the slow cooling of magnesium-rich and iron-rich magma into a holocrystalline mass deep beneath the Earth's surface. Slow-cooling, coarse-grained gabbro is chemically equivalent to rapid-cooling, fine-grained basalt. Much of the Earth's oceanic crust is made of gabbro, formed at mid-ocean ridges. Gabbro is also found as plutons associated with continental volcanism. Due to its variant nature, the term "gabbro" may be applied loosely to a wide range of intrusive rocks, many of which are merely "gabbroic". Contents 1 Etymology 2 Petrology 3 Distribution 4 Uses 5 See also 6 References 7 External links Etymology The term "gabbro" was used in the 1760s to name a set of rock types that were found in the ophiolites of the Apenn