仙境传说origin源码

㈠ 求一个简单的仙境传说RO的按键精灵脚本

1你要录制脚本
点击后切换到问道页面
按红色按扭开始 鼠标或者键盘 做你要录制的动作
在按 蓝色方格按扭 在保存
保存后进入 脚本录制器页面 在右边 有个运行
里面有个 脚本循环 选择循环发言时间
然后在按 保存推出 OK 选择你要播放的脚本
按F10 结束按F12 ==================以上是复制其他地方的答案，个人感觉按键精灵还是很简单懂的，你自己慢慢琢磨一下应该没什么难。

㈡ html5 rotete() 怎么设置旋转中心

-webkit-transform-origin: center bottom;
transform-origin: center bottom
transform-origin：[ <percentage> | <length> | left | center① | right
] [ <percentage> | <length> | top | center② | bottom
]?
默认值：50% 50%，效果等同于center
center
适用于：所有块级元素及某些内联元素
继承性：无
取值：
<percentage>：
用百分比指定坐标值。可以为负值。
<length>：
用长度值指定坐标值。可以为负值。
left：
指定原点的横坐标为left
center①：
指定原点的横坐标为center
right：
指定原点的横坐标为right
top：
指定原点的纵坐标为top
center②：
指定原点的纵坐标为center
bottom：
指定原点的纵坐标为bottom

说明：
设置或检索对象以某个原点进行转换。
该属性提供2个参数值。
如果提供两个，第一个用于横坐标，第二个用于纵坐标。
如果只提供一个，该值将用于横坐标；纵坐标将默认为50%。
对应的脚本特性为transformOrigin。

㈢ Ro ute Geological section of the Proterozoic in Jixian

Jixian County,an ancient county(previously Yuyang County)in North China,is located at the southern foot of the Yanshan Range and in the northern outer suburbs of Tianjin municipality.It is about 90 km east of Beijing and 100 km west of Tianjin.

Well-developed Proterozoic sequences crop out in the northern parto f the Jixian area(Fig.3-6).A NW-trending syncline with a core of Cambrian rocks occurs between Hongshuizhuang and Jing'eryu villages.A thrust fault parallel to the strike of the rocks between Yangzhuang and Chuancangyu villages caused a repetition of the strata.In addition,a large N-S trending fault from Huangyaguan to Yangzhuang with ENE-trending thrusts occurs along the front of the hill,north of Jixian(Fig.3-6).

The Proterozoic geology of the Jixian area and its vicinity was firsts tudied by Gao Zhenxi(C.C.Kao)et al.in 1934.These authors and many subsequent studies provided detailed descriptions of the lithology and subdivided the rocks into formations.They also properly identified the stromatolites occurring in the rocks.Based on these works,the Jixian section has been regarded as a typical section of the Middle and Upper Proterozoic in North China.

Fig.3-6 Geological map and cross-section of Jixian and adjacent areas

1—Quaternary;2—Cambrian;3—Jing'eryu Fm.;4—Luotuolingfm.;5—Xiamaling Fm.;6—Tieling Fm.;7—Hongshuizhuang Fm.;8—Wumishan Fm.;9—Yangzhuang Fm.;10—Gaoyuzhuang Fm.;11—Dahongyu Fm.;12—Tuan Shanzi Fm.;13—Chuanlinggou Fm.;14—Changzhougou Fm.;15—Archean;16—Pluton;17—Unconformity

At the beginning of the 1970's,the Proterozoic sequences around Jixian and Yanshan Range have been studied by many geologists,and numerous papers and monographs have been published on the lithology,paleontology,geochemistry,geochronology,paleomagnetism and paleogeography of these rocks.

The Proterozoic sequences in the Jixian area are underlain by Archean rocks and overlain by lower Cambrian strata.These sequences have a total thickness of 9193 m,which can be divided into 12 formations that define 3 systems,the Changcheng,Jixian and Qingkou systems.

Geochronological results date the Proterozoic sequences in Jixian area as ranging ca.1800 to 850 Ma.The Changcheng System is dated at ca.1800-1 600Ma,and the Jixian System at ca.1600～1000Ma and the Qingkou System at ca.1000-850Ma,and these systems belong to the late Paleoproterozoic,Mesoproterozoic and Early Neoproterozoic,respectively.The stratigraphic succession of these units is described as below:

1.The Late Paleoproterozoic Changcheng System

The Changcheng system con Sists of four formations with a total thickness of 2762 m.The lowermost Changzhougou Formation rests unconformably over the Archean metamorphic Zunhua Complex-Group,and is chiefly composed of conglomerate,pebble-bearing sandstone and arkosic sandstone of fluvial origin in the lower portion and sandstone of marine facies in the middle-upper part.The second formation,the Chuanlinggou Fm.,is mostly composed of neritic shales grading upward into the dolomitic Tuanshanzi Fm.The fourth formation,the Dahongyu Fm.,co nsists o f littoral and neritic sandstone,shale and K-rich trachyte with cherty dolo stone in the upper part.

(1)The Changzhougou Formation

Location:North top of Changzhougou(40°13′03″N,117°30′47″E,494m)

Content:Unconformity between Changzhougou Formation(Chch)and Archean(Fig.3-7).

Fig.3-7 Unconformity between Changzhougou Formation and Archean in Changzhougou

A—the unconformity of Chch/Ar;B—the river conglomerate and cross-bed in Chch

The Changzho ugo u Fo rmatio n,the lo wermost unit of the Changcheng System,co nsists o f grayish purple,massive to thick-bedded co nglo merate and co arse-grained sandsto ne,pinkish and white quartz sandsto ne,sedimentary quartzite and so me thin-bedded sandsto ne,fine-grained sandsto ne,clayey and feldspathic sand Sto ne with a thickness o f 859 m.The quartzite and quartzitic sandsto ne of shallo w marine o rigin are the chief co mpo nents o f the fluvial conglomerate,and coarse grained sandstone dominates in the lower part.

So far,no stromatolites have been identitied in this formation.However,a numbero fa critarches,including ssme unicellular eukaryotes,have been identified from the intercalated beds of muddy siltstone in the upper part of the formation.

（2)The Chuanlinggou Formation

Location:Chuanglinggou(40°11′52″N,117°28′50″E,295m).

Content:Boundary of Chuanglinggou Formation/Changzhougou Formation(Chc/Chch).

The Chuanlinggou Formation consists chiefly of silty and illitic lenses.It has a thickness of 889m in Jixian area,but much less in the eastern and western parts of the Yanshan Range.

This formation can be subdivided into three sections based on the quantity of sandstone and the color of rocks.The lower section of supratidal to intertidal origin is characterized by a large amount of yellowish-green sandstone,and the middle section is composed of black shale of subtidal to lagoonal facies with many intercalations of intertidal sandstone.Mud cracks are spectacularly developed and sand veinlets are common in the sandstone of the lower section.

Acritarchs are abundant in this formation and they include the following groups:Sphaeromorphida(e.g.Leiominuscula,Margominuscula,Dictgosphaera,Kildinellaand Leiosphaerida），Scaphomorphida(e.g.Dictgosphaera,Kildinellaand Schizovalvia），Versimorphida,including blade-like,lobe-like,valve-like and band-like forms(e.g.Pholimorphaaa,Lobomorphaand Valvimorpha）：and Nematomorphida(e.g.Qingshaniaand Changchengonema).In addition,some macroscopic,ribbon-shaped fossil algae have been reported.

There are no stromatolites in this formation in Jixian area,but two horizons containing stromatolites have been found in the western Yanshan Range.

(3)The Tuanshanzi Formation

Location:40°10′32″N,117°27′59″E,291m.

Content:Tuansanzi Formation/Chuanglinggou Formation(Cht/Chc).

The Tuanshanzi Formation is composed mainly of muddy and silty,micritic dolomite with a total thickness of 518 m(Chen et al.,1980).The lower member of this formation contains abundant muddy,silty and carbonaceous material,with pyrite impregnations and black carbonaceous films on the bedding planes.In the upper member,the content of clastic material increases considerably resulting in micritic sandstone,sandy dolostone,thin-bedded sandstone and small stromatolite bioherms.

The lower member of the Tuanshanzi Formation is characterized by even bedding indicating deposition in a quiet,weakly recing,subtidal environment(lagoonal facies）,whereas the upper part formed in an unstable environment probably between the intertidal and supratidal zones.Previously,the Tuanshanzi Formation was regarded as being poor in fossils,containing only a few of stromatolites,microfossils and doubtful megafossils dominated by Tyrasotaenia(Hofmann and Chen,1981).However,a large collection of megafossils represented by Iongfenshanids(Antiqufolia,gixianfolium and others)have been identified in the lower part of this formation in recent years,and interpreted as Paleoproterozoic megasc Opic eukaryotes Or metaphytes.

(4)The Dahongyu Formation

Location:40°10′28″N,117°28′00″E,258m.

Content:Dahongyu Formation/Tuansanzi Formation(Chd/Cht).

The Dahongyu Formation can be subdivided into two units.The lower unit consists mainly of white quartz sandstone and sandy dolostone,intercalated With purple and green tuffaceous siltstone or tuffaceous silty shale,locally accompanied by beds of volcanic breccia,tuffaceous sandstone and high-K lava.The upper section consists of micritic dolomite and cherty micritic dolomite with abundant stromatolites.A fe W poorly preserved acritarches have also been found mainly in the lower section of this formation.Some microscopic algal fossils occur in the cherty beds of the upper unit.

2.The Mesoproterozoic Ji Xian System

Disconformably overlying the Changcheng System,the Jixian system consists of five conformable formations with a total thickness of about 6088 m.The Gaoyuzhuang Formation at the base,is composed of littoral-neritic dolostone and dolomitic limestone.The overlying Yangzhuang Formation i S chiefly made up of alternating red-white marine dolostone with minor limestone.In the middle,the Wumishan Formation is composed of thick beds of siliceous dolostone intercalated with abundant cherty bands,and it grades upward into the Hongshuizhuang Formation composed dominantly of black shale.The uppermost Tieling Formation consists of shale and limestone with abundant stromatolites.

(5)The Gaoyuzhuang Formation

The Gaoyuzhuang Formation disconformably overlies the Dahongyou Formation of the Changcheng Group.Because it has sedimentary and paleontological characteristics typical of the“Jixianian System”.

This formation consists chiefly of carbonates and is subdivided into four members:

Member 1 is characterized chiefly by dark-gray cherty micritic dolomite,containing lenses of muddy and sandy dolomite.It also contains intercalations of thin-bedded,clayey,micritic dolomite and shale or silty shale.In addition,a bed of sandstone,about three meters thick,with ripple marks occurs at the base,where it overlies an erosional surface.

Member 2 could be further subdivided into two parts.The lower part consists of thin-bedded manganiferous,sandy micritic dolomite intercalated with dolomitic siltstone.Thick-bedded to massive dolomite with wavy bedding surfaces and large-scale ripple marks makes up the upper part of this Subformation.

Member 3 i S characterized by dark-gray muddy dolomite,calcareous micritic dolomite and dolomitic and micritic limestone with platy bedding,intercalated with some clastic layers and nolar limestone.

Member 4 begin S with dark,thick-bedded,calcareou S dolomitic micrite and dolomite,interca-lated with black,bituminous and muddy dolomite.This passes upward into gray,micritic dolomite with siliceous layers.All of these rocks in the upper part are thin-bedded and contain wavy bedding and cherty concretions.

The Gaoyuzhuang Formation contains various fossils.Stromatolites occur mainly in member 1 and are represented by Confusoconophytonmultiangulum,Gaoyuzhuangiacrassibrevis,G.Bulbosa,G.gaoyuzhuangensis,Tabuloconigera paraepiphyta,Conophyton garganicum and C.cylindricum.Microfossils interpreted as microscopic algae occur mainly in the cherty rocks of member 1.Although the microfossils are poorly preserved in the Jixian area,they are abundant in the same horizon in adjacent areas.Acritarchs are generally sparse and poorly preserved in the formation,and occur only member 1 and 3.The carbonaceous megafossils are represented by G.rvpaniaspiralis(namely Sangshuaniaspiralis,S.sangsuanensis and S.buccinata)and they occur only in the lower part of member 3.

(6)The Yangzhuang Formation

The Yangzhuang Formation consists of brick-red argillic,silty micritic dolomite with alternating white layers.Near both the base and top of the unit,there are thick layers of siliceous micritic or sparry dolomite.Many of the red layers have small,white spots.

This formation is subdivided into three members based on lithology.Both the lower and middle members contain ripple marks,mud cracks,cross-beds,and gypsum and salt casts indicating that they formed in supra-and intertidal lagoonal environments in a hot,dry climate.However,these features are absent in the upper member,which consists of bituminous dolostone.The Se rocks probably formed in a hot,wet,lagoonal environment.

Fossils are sparse and poorly preserved in the Yangzhuang Formation.Only some small stromatolites(Microstylus,Scyphus,Yangzhuangia)and a few achritarchs have been found in the lower and upper members.

(7)The Wumishan Formation

The Wumishan Formation,with a thickness of3336m,makes up one third oft he total Proterozoic section in the Jixian system.The rocks of this formation are rich in organic matter and show many cycles,suggesting deposition in a tidal environment.This formation includes four members:

1)The Lozhuang Member

The lower part of this unit contains alternating layers of white,muddy to silty,micritic dolomite,banded cherty micritic and sparry dolomite with intercalations of bituminous dolostone.The upper part is composed mainly of gray and dark-gray,medium-to thick-bedded,sparry dolomite with bands of chert and black,bituminous dolostone.These microbial deposits are characterized by small,wavy,laminated and columnar stromatolites.

2)The Mopanyu Member

This member consists chiefly of white silty to shaly micritic dolomite and thick-bedded stromatolitic,sparry dolomite.Chert layers,chert concretions and flat-pebble cherty conglomerates occur in the lower part of the unit.The upper part contains some thick-bedded,bituminous sparry dolomite with wavy laminae of algae,with several large,conic stromatolitic and silicified oolitic beds atthe top.

3)The Ershilipu Member

This member is subdivided into a lowera nd an upper parts.The lowerp art consists of white,rhythmically layered shaly to silty micritic dolomite,gray calcareous to muddy dolomite and gray，calcareous micritic dolomite with layers of black chert.Red,shaly,silty or sandy micritic dolomite occur in the base of the lower unit.The upper part generally consist S of dark-gray and thick-bedded calcareous,micritic dolomite.

4)The Shanpoling Member

This member can be subdivided into al owera nd an upperp arts.The lowerp arti s composed of gray to grayish-white,calcareous,micritic dolomite and cherty micritic dolomite intercalated with bituminous dolostone.The upper part consists mainly of light gray,thin-bedded calcareous,micritic dolomite without chert.In addition,a bed of white dolomitic sandstone occurs at the bottom of the formation in the Jixian area,and a bed of glauconite-bearing stromatolite dolostone,several tens of meters thick,occurs at the top.

The Wumishan Formation contains abundant stromatolites and microscopic fossil algae.In addition to large varieties,there are many small stromatolites in this formation,namely Psoudogvmnosollen moponyueuse,S'chuphus parvas and Mlcrostylus deusus.These mini-stromatolites occur mainly in the Lozhuang(1 st)member and the lower part of the Ershilipu(3rd)member.The larger varieties,represented by Conophyteslituum,C.shanpolingese，Jacutophytonfurcatum and Colonnelladiscreta,occur mainly in the Mopanyu(2nd)member and the upper part of the Ershilipu(3rd)member.Some medium-sized stromatolites,such as Pseudochihsienela,Wumishanellaand Paraconophyton,occur at the top of the Shanpoling(4th)member.A multitude of fossil algae have been found in the black cherty layers of this formation.The most important are Palaeolynbya,Sphonophycus,Eoentophysalis,Oscillatoriopsis,Sacdyngbya,Hyxococcodes.Harythrixand Archeaoellipsotdes.In addition,Some eukaryotic algae,Such a S Pandorinepsis,Uronemopsi,Hyalothecopsis and Templuma,Pseudochihsienela,Wumishanellaand Paraconophytonare also present.

(8)The Hongshuizhuang Formation

This formation is only 131 m thick and is subdivided into a lowera nd an upper members.The lower member is composed of grayish or dark yellow,thin-bedded,muddy dolostone with some intercalations of black and green shale.The upper member is dominated by black and green shale containing very fine silty laminations.Al1 of these sediments were probably formed in a lagoon or bay.Many distinctive acritarchs with quadrangular,triangular,global and scaffold forms,such as Quadratimorpha,Triangumarpha,Leiofusa,Scaphida,Trachysphaeridium and Pseudezonosphera have been reported by Xing and Liu(1973).In addition,a few of filamental forms and carbonaceous megafossils such as Chuaria are also present.

(9)The Tie Iing Formation

The Tieling Formation,the uppermosts tratigraphic unito ft he Mesoproterozoic Jixian System,consists of two members:the lower shale member and the upper limestone member,which combined total about 330m in thickness.Based on the existence of a layer of“ferruginous sandstone”，a disconformity was formerly thought to exist between the two members.However,recent study shows that the“ferruginous sandstone”and associated rocks may simply be the procts of hydrothermal alteration.This layer,about 2m thick,consists ofjasper and Mn-bearing,dolomitic limestone.

Microscopic acritarchs and stromatolites have been found in the lower shale member and the upper limestone beds,respectively.The stromatolite S are very well developed and constitute a“stromatolitic palace”（Fig.3-8)in the Jixian area.They are represented by Kussiella,Scopulimorpla,Anabaria,Baicalia,Tielingellaand Chihsienella.The Tieling Formation i S disconformably overlain by the Xiamaling Formation,which belongs to the Neoproterozoic Qingkou System.

Fig.3-8 Stromatolites are very well developed in Tieling Formation

A—shape in longitudinal thin section;B—shape in transverse thin section

3.The Qingkou System

This system includes three formations,which constitute two integrated sedimentary cycles.The Xiamaling Formation,which consists of conglomerate,sandstone and shale,disconformably overlies the Tieling Formation,and is overlain by conglomerate,arkosic sandstone,glauconitic sandstone and shale of the Luotuoling Formation.The uppermost unit,the Jingeryu Formation,con Sists of limestone.The Qingkou System has a total thickness of 370 m and is disconformably overlain by the Cambrian Fujunshan Formation.

In the Jixian area,as in the mostp arts of North China,there was no sedimentation untilt he middle of the Early Cambrian.

(10)The Xiamaling Formation

A 168-m-thick layer of yellowish-green to grayish-green,clayey siltstone with lenticular sandstone beds disconformably overlying the Tieling Formation,is named as the Xiamaling Forma-tion after its original locality in the western Hills of Beijing(compare this with Stop 6in Route 2).These rocks have current marks,such as furrow casts and groove casts on the sandstone bedding planes along with mud cracks,suggesting deposition in a supratidal or intertidal environment.

Abundant acritarchs,such as Microconcentrica,Gloeocapsomorpha,Symplasso-sphaerdium and Tasmanites,have been recovered from the silty shales.These acritarchs have shapes and ornamen-tation that distinguish them from those in the underlying strata.

（11)The Luotuoling/Changlongshan Formation

This formation was formerly considered to be the lowerp arto ft he Jing'eryu Formation,and was designated the Changlongshan Subformation(Chen et al.,1980).Wang et al.(1980)named it the Changlongshan Formation,whereas Xing et al.(1989)suggested the name Luotuoling Formation after its type locality in the Jixian area.It disconformably overlies the Xiamaling Formation in the Jixian area or other older horizons in adjacent areas,and conformably underlies the Jing'eryu Formation.

The Luotuoling Formation,which is 118 m thick,begins with basal conglomerate followed successively upward by green and yellowish-green shale and glauconite-bearing,arkosic sandstone.The upper part of the formation is characterized by purple,gray and black shale.Two types of glauconite are present in the sandstones,a granular variety distributed along cross-bedding planes and interstitial cement.

(12)The Jing'eryu Formation

The Jing'eryu Formation was formerly designated as the upperp arto ft he“Jing'eryu Formation”（Chen et al.,1980),but many workers regard it as an independent formation.This unit is only 100 m thick in the Jixian area and consists mainly of variably colored limestone.The color changes successively upward from red,to grayish-green,light green,and grayish-brown to green at the top.Based on its sedimentary structures,these rocks were deposited in a subtidal environment.

The Jing'eryu Formation is disconformably overlain by the middle-lower Cambrian Fujunshan Formation,which contains a trilobite fauna of Redlichiachinensls(Walcott)and Megapalaeolenus fengyangensis(Chu)in dolomitized limestone.

㈣ 在电脑玩ro origin登录不了谷歌账号，是什么问题呢

现在很多游戏都是通过Origin平台下载和游玩游戏，Origin平台用户也越来越多，但是Origin也偶有系统不稳游戏不能登陆的情况，这种情况要怎么解决呢？

工具/原料

• Origin平台

• 电脑

方法/步骤

• 1

  1.当我们打开电脑上Origin游戏平台

  

• 8

  8.轻松进入游戏了。即使页面登陆不了，我们也可以换条路径到达哟，毕竟条条大路通罗马嘛！希望对您有帮助哟！

㈤ matlab里rotote什么意思

rotate 函数在三维空间中旋转图形对象。

rotate(h,direction,alpha) 将图形对象 h 旋转 alpha 度。指定 h 为曲面、补片、线条、文本或图像对象。direction 是一个二元素或三元素向量，它与旋转轴原点共同确定旋转轴。旋转轴的默认原点是图框中心。该点未必是坐标区的原点。

正 alpha 定义围绕方向向量从旋转原点伸展的右旋角度。

如果 h 为句柄数组，则所有对象必须为相同坐标区的子级。

rotate(...,origin) 将旋转轴的原点指定为三元素向量 [x0,y0,z0]。

㈥ rectrospectively是什么意思

retrospectively (法律, 付款等)有追溯力的

spelling wrong

㈦ 谁制作出了第一个网络游戏

这篇文章实在是枯燥，一直没有摆出来，毕竟这是一个宏大的话题，比较俗套，但是每日慌度于虚拟世界中的我们，是否应该回忆一下呢？今天让我们整理一下思绪，看看自己的过去,过去陪伴过我们的网络游戏，以及过去没有玩过的网络游戏……

世界上第一款网络游戏：1969年，一名叫瑞克·布罗米的美国人为PLATO远程教学系统编写了一款名为《太空大战》的游戏，该游戏以诞生于麻省理工学院的第一款电脑游戏《太空大战》为蓝本，可以支持两人远程连线，有趣的是，1969年也正是ARPAnet（Advance Research Projects Agency Network）诞生的年份。大家知道，ARPAnet是美国国防部高级研究计划署研制的世界上首个包交换网络，它的成功直接促成了互联网以及传输控制协议（即TCP/IP）的诞生，不过这款游戏至今被人遗忘在角落里，现在估计国内玩家没有几个知道吧。

1978年英国的埃塞克斯大学，罗伊·特鲁布肖用DEC-10编写了世界上第一款MUD游戏——“MUD1”，拥有20个相互连接的房间和10条指令，用户登录后可以通过数据库进行人机交互，或通过聊天系统与其他玩家交流。网络游戏出现了"可持续性"的概念，玩家所扮演的角色可以成年累月地在同一世界内不断发展，而不像PLATO上的游戏那样，只能在其中扮演一个匆匆过客。游戏可以跨系统运行，只要玩家拥有电脑和调制解调器，且硬件兼容，就能连入当时的任何一款网络游戏。

1984年马克·雅克布斯组建AUSI公司（《亚瑟王的暗黑时代》的开发者Mythic娱乐公司的前身），并推出游戏《阿拉达特》（Aradath）。雅克布斯在自己家里搭建了一个服务器平台，安装了8条电话线以运行这款文字角色扮演游戏，游戏的收费标准为每月40美元，这是网络游戏史上第一款采用包月制的网络游戏，包月制的收费方式有利于加速网络游戏的平民化进程，对网络游戏的普及将起到重要作用。遗憾的是，包月制在当时并没有成长起来的条件，1990年AUSI公司为《龙门》（Dragon's Gate）定的价格为每小时20美元，尽管费率高得惊人，但仍有人愿意每月花上2000多美元去玩这款游戏，因此在80年代末90年代初，包月制并未引起人们的关注。

1991年Sierra公司架设了世界上第一个专门用于网络游戏的服务平台--The Sierra Network（后改名为ImagiNation Network，1996年被AOL收购），这个平台有点类似于国内的联众游戏，它的第一个版本主要用于运行棋牌游戏（当时的比尔·盖茨是一名狂热的桥牌手，在Sierra Network上拥有自己的账号，且常常光顾），第二个版本加入了《叶塞伯斯的阴影》（The Shadow of Yserbius）、《红色伯爵》（Red Baron）和《幻想空间》（Leisure Suit Larry Vegas）等功能更为复杂的网络游戏。当时Sierra Network的运营者还曾同理乍得·加利奥特联系，希望把开发中的《网络创世纪》搬到Sierra Network上。随后几年内，MPG-Net、TEN、Engage和Mplayer等一批网络游戏专用平台相继出现。

相信资深一点的网游玩家都会知道网络游戏的雏形——MUD，MUD是一种文字类的游戏，通过输入命令来进行动作，当然动作的展现形式也是文字叙述，游戏中充满了刺激与快感，可以说文字MUD是一种“会动的小说”，你就是那小说中的主人公。提起文字MUD，国内的玩家都会不由的想起“武侠”，没错，初期，国内的文字MUD大多数以武侠为主题，这跟我们的国情是不可分割的，想想看当你可以在金庸、古龙等武侠世界中闯一片天下，那是让人何等快乐的事情。于是国内的方舟子和翔少爷于1996年1月建立了mud《侠客行》，这款游戏成为国内文字MUD的代表，几乎任何一个MUD爱好者都没有错过。随后99年4月乐斗士工作小组正式成立，经过对原电话游戏的升级改造，推出了国内最早的简易图形MUD游戏———《笑傲江湖之精忠报国》，但当时图形MUD已经有所规模，文字MUD面临衰退。

2000年7月 第一款真正意义上的中文网络图形Mud游戏《万王之王》正式推出，凭借优秀的游戏质量，配合特殊的历史条件，《万王之王》成为中国第一代网络游戏无可争议的王者之作。中国网络游戏的运营机制也通过《万王之王》得到了建立，而其诱出的潜在市场成为吸引更多公司冲击网络游戏市场的直接原因。两个月后智冠也随之推出《网络三国》与同期的《万王之王》分庭抗礼，并且赢得了不错的口碑。

2001年1月，华义推出了来自日本的网络游戏《石器时代》一举打败所有网游，网络游戏玩家纷纷涌入，相信大多数的网游老玩家都是从此时开始的，《石器时代》推出的时机正式国内互联网普及的时期，网吧日益增多，成为唤醒国内网游玩家的网络游戏。同年3月，亚联、台湾圣教士、晶合时代共同推出韩国武侠网络游戏《千年》，因为背景与中国文化更为接近，使得其成为早期韩国网络游戏中最具影响的作品，为韩国网游进军内陆打下了突破口，随后韩国的龙族、红月纷纷涌入国内市场，年底，网易推出了其筹划已久的国内原创网络游戏《大话西游》吹响了门户网进军网络游戏产业的号角。这一举措让网络游戏成为了门户网新的利润增长点。

此时，上海盛大《传奇》踏入网游市场，当时并没有取得很好的效果，但是谁也想不到的是，就是这款当时看似不入流的网络游戏在三年内称霸于国内网游市场，原因很简单，国内网民的迅速增长，其他网游的衰退，都是《传奇》成功的关键。

2002年，由于《传奇》的成功，韩国网络游戏纷纷进入国内，顿时百花齐放，网游界一片混乱。随后传奇私服外挂横行，《传奇》衰退，玩家转战其他网游，韩国的《奇迹》、《仙境传说》等仍然是国内网游的主角。年底，网络游戏产业链初步形成，国内厂商觉醒。

至今的三年内，国内推出网络游戏已达约200款左右，网游玩家已达2633万人，市场规模巨大。

网游市场仍在以飞速发展，《魔兽世界》的诞生刺激了欧美网络游戏，盛大亦将代理《龙与地下城OL》。未来网络游戏市场会怎样，没人感预计，但是可以肯定的是，这群致力于网游的国内代理、开发厂商们，还是会继续赚到腰包爆掉，让我们静静的看吧。